5ZC16SEMC5 63.46*8 BENNETT 010
Of 2.
LYNX-CANADA EXPLORATIONS LTD.
SPARTON RESOURCES INC.
BENNETT LAKE PROPERTY
Prepared by: Peter Mordaunt Randy Crowley
For; Lynx-Canada Explorations Ltd, Sparton Resources Inc.
S2C16SE*M6 63.4AM BENNETT 010C
TABLE OF CONTENTS
INTRODUCTION..........................SECTION l
MAGNETIC SURVEY.......................SECTION 2
ELECTROMAGNETIC SURVEY................SECTION 3
GEOLOGICAL SURVEY.....................SECTION 4
GEOCHEMICAL SURVEYS...................SECTION 5
TRENCHING.............................SECTION 6
DIAMOND DRILLING......................SECTION 7
CONCLUSIONS...........................SECTION 8
REFERENCES. . .... .... ................. .SECTION 9
SECTION l
INTRODUCTION
This report is presented to fullfill the requirements of The Ontario Mineral Exploration Program Act,1980 in Application for Grant or Certificate of Entitlement to Tax Credit for Designated Program OM83-3-C-SW.Application is made in the name of: 35^.,
LYNX CANADA EXPLORATIONS LTD. 520-25 ADELAIDE STREET EAST TORONTO,ONTARIO
LOCATION and ACCESS
The claim group is located north of Bennett and McPherson Lakes on the Bennett Township map sheet (M-1920), in the Kenora Mining Division.
The property lies midway between Atikokan and Fort Francis approxiraatly 6km north of Hiway #11.The town of Mine Centre is the closest populated centre where supplies may be purchased.
Access to the claim group is via bush road from Hiway #11 to either Bennett Lake or McPherson Lake then by boat and/or foot to the claim group. Camp is established at McPherson Lake in a cottage rented from Mr.Ted LaBelle, Sapawee.
PROPERTY
The Bennett Lake claim group consists of 65 unpatented mining claims as follows:
K759817 l K759821 - K759750 inclusive 30 K759777 - K759795 inclusive 19 K676190 - K676196 inclusive 7 K655361 - K655368 inclusive 8
All claims are recorded in the Kenora Mining Division on plan M-1920, Bennett Lake
GRID-LINECUTTING
An exploration grid totalling 116km has been established to cover all claims..Line spacing is 100m with stations established at 25m intervals.The baseline trends east-west from L32+OOW to L22+OOE and trends 45 degrees from L22+OOE to L40+OOE. A detailed grid was cut for follow-up geophysics from line 19 west to line 27 west. This grid was cut with 50 meter spacings and centres. Even closer grid lines were cut with 25 meter spacing and centres
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23-27 west.
SUMMARY OF EXPLORATION
This report details the results of a major exploration program undertaken by Lynx Canada Explorations Ltd.Surveys include complete coverage of all claims with linecutting,VLF-EM,magnetometer,soil and humus surveys.Prospecting and a geological survey was completed on the western half of the property. A detailed grid described above was the focus for follow-up geophysics includ ing magnetometer and VLF-EM. Furthermore,a trenching program occured as a result of a promising gold showing. In addition to the above work four diamond drill holes were drilled for a total of 1274 feet.
PREVIOUS WORK (1)
1896-1899: Developmental work first began on the property in 1886. Several test pits and a shaft was sunk to 75 feet (23 metres) with 20 feet (6 metres) of drifting arid 13 feet (4 metres) of crosscutting at the 45-foot level (14 metres) were completed. In addition, on the north shore of Bennett Lake (formerly Cedar Lake) a 16-foot adit (5 metres) was driven northward. A five stamp mill was erected in 1898 through which 125 tons of core were milled All the work was completed by the Independence Mining and Development Company Ltd. No further exploration work is known to have taken place on this property.
1910: The patented claims which were surveyed in 1897 lapsed in 1910 and became open ground.
1915: The property was acquired by J.A. Kennedy, .et al.
1980: The property was visited by S.L. Fumerton of the Ontario Geological Survey and 11 sampled and detailed geological mapping is completed. At that time, the property was held by R.J. McLean Jr. , E . Walton, M.J. Strangis, A.E. Dalby, and J.W. Richardson.
1982: The property was visited by the Atikokan Economic Geologist Program where sampling was conducted.
General Geology and Structure of Independence Mine:
The Independence Mine is structurally situated (within 0.5 km) north of the Quetico Fault. The area is underlain by steeply dipping, west striking felsic to mafic metavolcanics. The metavolcanics are composed of sericite- chlorite-carbonate schist which may have originally represented a felsic fragmental rock, such as a tuff of lapilli tuff which underwent intense shearing and silicification. These felsic tuffs are intercalated with mafic tuffs and epiclastic and chemical metasediaents. Fumerton (1981) describes the country rock as a felsic quartz crystal tuff in which the quartz clasts commonly have a blue tint.
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learing is prominent throughout the Independence Mine property, striking east-west with near vertical dips.
Mineralogy of the Independence Mine:
The main quartz vein was reported by Bow (1699) to be up to 60 feet (18 metres) in length on surface and.up to 2 feet (0.6 metres) wide. Fumerton (1961) indicated that there are numerous small, discontinuous quartz veins occurring at various attitudes within a host rock of felsic tuff. The veins appear to be associated within east-west trending lenticular shear zones. Visible mineralization consist of pyrite, chalcopyrite, galena, sphalerite and gold; with accessory minerals including sericite, chlorite and carbonate.
The principal workings of the Independence Mine exploited narrow and dis continuous quartz veins in a sheared quartz crystal tuff.
Tonnage and Grade Estimates:
None recorded.
Past Production:
During 1698, Independence Mining and Development Co. Ltd. produced 121 ounces of gold from 125 tons of ore giving a grade of 0.97 ounces of gold per ton. (Ferguson et al, 1971)
Chemical analysis of the Independence Mine:
Bow (1899) reported alleged gold values of 0.39 ounces per ton in the host rock adjacent to the main quartz vein, which contains erratic gold miner alization of up to 7.76 ounces gold per ton. Eight selected grab samples from a rock dump near the shaft were collected by Fumerton (1981) giving values obtained from samples of quartz vein material from trace to 0.96 ounces gold per ton. A sample of the host rock, barren of sulphide mineralization, contained trace amounts of gold, whereas host rock samples with some sulphide mineralization contained between trace and 0.04 ounces gold per ton. Twelve samples collected from the adit on the north shore of Bennett Lake contained trace amounts of gold.
Samples collected by the Atikokan Economic Geologist Program gave low results.
- 4 -
SECTION 2
MAGNETIC SURVEY
Instrumentation
The survey was performed by Phanton Exploration Services Ltd.using a Scintrex MP-2 portable proton-precession magnetometer.A Scintrex MBS-2 magnetic base station was used to record and correct for diurnal variations.
The MP-2 has an accuracy of +/-1 gamma in a field of 50,000 gammas.' However,actual survey accuracy is proportional to the degree of care used in applying diurnal corrections.
Theory of Operation
Magnetic variations are caused by variations in magnetization of the rock from station to station.This magnetization exists because of the presence of minerals with high magnetic susceptabllity.The most common minerals to affect the earths magnetic field are magnetite,pyrrhotite,and ilmenite. Magnetometers are used to measure this variation.
The MP-2 is a proton precession magnetometer.This magnetometer utilizes the precession of spinning protons in a volume of kerosene to measure the total magnetic field intensity.
When the hydrocarbon is subjected to an electric current the spinning - protons are temporarily polarized.When the current is removed the spin of the protons causes them to precess about the direction of the ambient magnetic field.The signal generated by the processing protons is directly proportional to the intensity of the total magnetic field.The magnetic intensity measured is the magnitude of the earths magnetic field vectorindependant of its direction.A change in the total field intensity is referred to as an anomoly.
Survey Procedure
Data was collected at 25m intervals using a Scintrex MP-2 proton magneto meter. Field data was then referred to the log of a base station recorder { Scintrex MBS-2 ) which operated continuously throughout the survey for correction.The corrected data is plotted at a scale of 1:2500 and contoured.
Discussion of Results
A large number of magnetic anomolies were identified over the four map sheets covering the claim group.The following tables indicate the location, strike length,strength,possible source and conductivity of any associated EM conductor.
- 5 -
[G magnetometer survey proved usefull in sorting-out the various types of iron formation present on the property.The sulphide facies iron formation usually has a magnetic signature of 2000-5000 gammas,the magnetite iron form ations have a magnetic signature between 6000 and 21000 gammas.There are many magnetic highs on the property that show no VLF response,these may may be due to non-conducting magnetite bearing flows or sediments.
The background magnetics are lower on the eastern part of the grid than the west.
Detailed Magnetometer Survey
A detailed grid was cut for the purpose of follow-up geophysics. A coincident VLF and mag. anomaly (le.flanking) between lines 23-27 west was clearly defined and outlined as a result of detailed readings. The anomaly is explained as magnetite and pyrrhotite which were observed in drill holes number one and two.
Another coincident anomaly to the south (ie.L-2H/1+75S) was also drilled (BL-3-84).This hole revelled pyrrhotite and this is thought to be the cause of the magnetic anomaly. Other magnetic responces within the detailed area appear to be isolated with a general trend east-west. This east-west trend was exspected based on the local strike outlined by the geological survey.
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SECTION 3
ELECTROMAGNETIC SURVEY
Instrumentation
A VLF-EM survey was performed by Phantom Exploration Services Ltd.using a Geonics EM-16 unit.
Theory of Operation
VLF-transmitting stations operating for military communication have vert ical antenna.The vertical antenna creates a concentric horizontal magnetic field .When these magnetic fields encounter conductive bodies in the ground, a secondary field is created.The VLF receiver measures the vertical components (inphase and quadrature) of these secondary fields.
The EM-16 is a sensitive receiver covering the frequency bands of the VLF-transmitting station with means of measuring the vertical field components.
The receiver has two inputs,with two receiving coils built into the instrument.One coil has normally vertical axis,the other is horizontal.
The signal from one of the coils (vertical) is first minimized by tilting the instrument.The tilt angle is calibrated in percent.The remaining signal in this coil is finally balanced out by a measured percentage of a signal from another coil,after being shifted by 90 degrees.
Thus if the secondary signals are small compared to the primary horizon tal field,the mechanical tilt angle is an accurate meaure of the vertical real-component,and the compensation 90 degree signal from the horizontal coil is a measure of the quadrature vertical signal.
Survey Procedure
Readings were taken at 25m intervals over the entire grid.Both the dip angle and the quadrature were noted at each station.The transmitting station used was Cutler,Maine.
To take a reading the refrence coil ("T") in the lower end of the handle is oriented along the magnetic lines 90 degrees to the station direction.This is acheived by swinging the instrument back and forth until a minimium sound intensity is heard.The quadrature dial is then adjusted until the sound is further minimized.The dip is then read from the inclinometer and the
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quadrWure from the dial.The same direction is always faced when readings are taken.
Discussion of Results
A total of 81 EM-16 anomolies were identified over the four map sheets that cover the claim group.The following tables provide the location,strike length,fliter response (Fraser Filter),conductivity,magnetic response,and remarks on possable source.
Many EM-16 conductors are due to topographic features such as drainage and cliffs.However,the EM-16 did detect numerous bedrock conductors.The EM-16 detected a number of sulphide and magnetite rich iron formations as well as conductive zones with no associated magnetic signature.
The quadrature l in-phase ratios are a good check on the apparent conduct ivity of the anomolies and proves usefull in classifying the conductors.The VLF responses were between weak and moderate with very few anomolies of high conductivity.
Detailed Electromagnetic Survey
In the fall a detailed grid was cut for both mag. and EM follow-up surveys The detail was concerned with better definition of anomaly "N" (see previous section).Results from this survey outlined a good to moderate responce with a strike length of 375 meters. This responce was thought to be caused by a sulphide bearing horizon which drill holes one and two confirmed.
Other anomalies although not as strong in responce or over as great a strike length were also defined more clearly.Drill hole number four tested a strong EM responce from L-24+50W to L25+50W at 1+75S. There were sufficient sulphides in the dril core to explain this EM conductor.
MAP
1
1
1
1
1
1
1
1
i
A
8
C
D
E
F
H, G
HH
LOCATION
28vEast 1H50 S
29Erto 30E 2+50S
27E to 29E 0+65S
24E 2^ 60S
23E 0+65S
2UE 0+85N
26E to 28E 2+65N
25E 2+90N
STRIKE LENGTH (meters)
0 to 100
100 to 200
200 - 300
0 to 100
0 to 100
0 to 100
100 - 200
0 to 100
FILTER RESPONSE
STRONG
*;-jr FAIR
WEAK
STRONG
STRONG
WEAK
STRONG TO WEAK
STRONG
CONDUCTIVITY
POOR
POOR
POOR
POOR
POOR-
POOR
POORV
POOR
MAGNETICS (GAMMAS)
2000
FLANKING
FLANKING DIPOLE
NONE
NONE
NONE
NONE
NONE
REMARKS
SWAMP?
SWAMP Y, HAS A 2000 GAMMA MAG FLANKING IT
1900 GAMMAS
SWAMP EDGE
SWAMP?
TOPOGRAPHY?
OPEN MARSH
AS ABOVE
HAP
1
1
1
1
1
1
1
f
I
J
K
L
M
N
0
LOCATION
29E to 30E 1+75N
33E to 34E 1+35N
38E 0+50N
28E to 3?E1+50 - 3+oor
37E 3+50N
35E 8+OON
31 E to 34E 7+25N
STRIKE LENGTH (meters)
0 to 100
100 - 200
0 to 100
900+
100+
0 to 100*
300+
FILTER RESPONSE
WEAK
PAIR
STRONG
WEAK TO STRONG
MODERATE
WEAK
WEAK
CONDUCTIVITY
POOR
POOR
MODERATE
MODERATE TO GOOD
MODERATE
POOR
MODERATE TO GOOD
MAGNETICS (GAMMAS)
NONE
2900
FLANKING (1200)
3-4000
6000
Minor 300 Gam -ma low
2500
REMARKS
SWAMP? POSSIBLE EXTENSION OF "J"
Best response on lines 28E and 30E(3-4000garamas mag) Majority of conductor cor relates to an open marsh and swamp.
Open to the east. VLF enhanced by the lake.
Mag only on the one line (31E). There is a possibly of two different con ductors .
-
MAP
2
2
2
2
2
2
2
f
A
B
C
D
E,F
G,G(
H
LOCATION
5E to 6E5-75S
7E -o 8E7*5O to 8+00South
1CI to 1*4-E' r DOS
1JE to l^Ei-oOS
5E 5+OOS6E 6+OOS
r 5E -ro 18E;-5DS
172
STRIKELENGTH(meters)
0 to 200
100 to 200
200*
150*
0 to 100
1300+
0 to 100
FILTER RESPONSE
Strong
Strong
Strong
Strong
Weak
Strong
Weak
CONDUCTIVITY
Moderate
Good
Good
Poor
*
Poor
Poor
Poor
MAGNETICS(GAMMAS)
3100
2000
If- 8000
Flanking?(2100)
None
Spot Highs
None
REMARKS
These conductors areprobably all due to thesame folded magnetiteiron formation along theshores of McPhearson Lake.The conductor seems totruncate around 12E
Swamp?
Corresponds to an opendrainage system whichhas enhanced the VLF re sponse. Mag correlation onlines 5E and l^E.
Swamp?
MAP
2
2
2
2
2
2
f
I
II
J
K
L
M
LOCATION
18E to 20E 1+OOS
21E to 22E BL to 0+251^
13E to 15E 0+25N
5E to 6E 0+35S
5E to 22E
18E to 22E 5+OON
i
STRIKE LENGTH (meters)
300+
100 - 200
100 - 200
100 - 200
1700+
1*00*
FILTER RESPONSE
Strong
Weak
Weak
Strong
Strong
Strong
CONDUCTIVITY
Moderate to Coot
Podr
Poor
Poor
Moderate
Moderate
-
MAGNETICS (GAMMAS)
None
2000
Yes
None
Spot Highs
None
REMARKS
Swampy ground has en hanced the V1P response however the conductivity upgrades this conductor
Mag and shorter strike make this interesting
Has a moderate dipole (120-2^00 gammas) with it
Swamp?
VLF response enhanced by swamp t Mag correlation on lines 5E,6E,10E to 12E, H*E to 15E, 17E to 22E. A very high nag (9000) probably due to magnetite
VLF enhanced by swamp
'
SAP
2
2
2
r 2
a
3
;i 3
f
N
0
P
Q
R
A
B
LOCATION
12E 5+OON
5E to 16E 9+OON
7E 8+25N
5E 10+50N
7E to HE 10+50N
12W to 15W 6+50S
10W - HW 7+50S
STRIKE LENGTH (meters)
0 to 100
1100+
0 to 100
0 to 100
too*
300 to 350
200 - 300
FILTER RESPONSE
Fair
Strong
Strong
Strong
Strong
Strong
Weak to Moderate
CONDUCTIVITY
Poor
Poor to Moderate
Moderate
Poor
Poor
Moderate
Poor
MAGNETICS (GAMMAS)
None
Yes (2000)
Yes
None
Yes
Questionable
None
REMARKS
Lake effect
A series of dipoles along the strike length of this conductor suggests a pinch and swell morphology. Maybe a sulphide iron formation.
A minor low (200) flanking it.
Beaver swamp.
Mag correlation on lines 9E to HE (2000), sulphide iron formation? V1F en hanced by the swamp edge.
Very strong VLF (swamp?) Mag correlation is incon clusive .
"A- 4 "B" are probably the same conductor
MAP
3
3
3
3
3
3
3
#
C
D
E
F
G
H
I
LOCATION
5W to ?W 7+50S
3E to 1W 6+50S
1W to 13W 3+00 - 5+00
IE to 1W i**50S
J*EJ++50S
0 to kE 1+50 to 300s
IE to 3E 1+OOS
STRIKE LENGTH (meters)
200 to 30(
300 tolfOO
1200+l
200 to 300
0 to 100
1*00 to 500
200 to 300
FILTER RESPONSE
Weak
Moderate to Strong
Moderate to Strong
Fair
Moderate
Strong
Moderate
CONDUCTIVITY
Poor
Poor
Poor to Fair
Poor to Fair
Poor
Poor
Poor
MAGNETICS (GAMMAS)
None
None
Questionable
Yes
None
Questionable
None
REMARKS
Swamp?
Possible mag on 2W. Swamp system causing much of VLF
A very long conductor which swampy topography. Mag suggests correlation (how ever VLFcuts across; the mag trends in some cases t
Line 0 has a mag low(2?7)
V1F response flanks a 5**00 gamma high on line 3E* How ever there was no VLF on that line.
VLF response follows an open marsh.
Swamp edge?
MAP
3
3
3
3
3
3
3
3
#
J
K
KK
L
M
N
0
P
LOCATION
1W 0+50S
3W to 12W baseline
5W to 6W 0+25N
HW to 12W 0+75S
13W to 15W 2+50S
13W1+OON
HW to 12W 2+OON
7W-8W-9W 2+OON
*
STRIKE LENGTH (meters)
0 to 100
1200 - 130C
100 to 20C
200 to 30C
200 - 300
0 to 100
100 to 20(
0 to 100
FILTER RESPONSE
Moderate
Moderate
Moderate
Moderate to Stror
Moderate to strong
Strong
Strong
Weak to Moderate
CONDUCTIVITY
Poor
Moderate to Poor
Moderate to Poor
g Moderate
Poor *
Poor
Moderate
Weak
MAGNETICS (GAMMAS)
None
Yes
Yes
Questionable
Yes(2500)
Flanking dipole
Ye s (30 00)
Yes (4000)
REMARKS
2500 gamma mag along the BI (sulphide Iron formation?)
Same as "K"
VLF enhanced by a creek am its marshland.
VLF the same as "L" but has mag associated with it.
Sulphide Assemblage?
Possible Iron Formation (sulphide)
A group of three one line VLF responses with the bes* being on line ?W. This cor relates with a *K)00 mag hi, high. (sulphide IF)
MAP
3
3
3
3
i
Q
R, S
T
U
LOCATION
2E to 4W2+00 - 3+OON
^E to HWJHOO - 6+OON
^E to 1W7+00 - 8+OON
12W to l^W5+OON
STRIKELENGTH(meters)
600 to 700
1500 - 160
500 to 600
0 to 100
FILTER RESPONSE
Strong -
) Strong
Moderate to Stron
Moderate to Strong
CONDUCTIVITY
Poor to Moderate
Poor to Good
l Poor to Moderate*
Moderate to Good*
*
MAGNETICS(GAMMAS)
Questionable
Yes (2-22000)
Questionable
Questionable
REMARKS
VLF enhanced by swamp. Runsparallel to a long ironformation to the north ("R"and "S")
Characterized by a seriesof dipoles along its strikelength. Extremely high magvalues, probably due to amagnetite bearing IF. R& Sare grouped because they azprobably the same horizon.
Mag data indicates a highon line 2E however this majibe due to a mafic intrusiverather than the conductor.
A number of VLF responseslie within a broad mag highThis could be due to localfolding of the IF describeefor "R" it " S".
*
MAP
4
k
k
4
4
#
A
B
C
D
E
LOCATION
2?W to 32W10+00 - 11+00
South
32W to 33W8+50S
. 30W' v: 8*50S
31W to 3^W5S to 8S
21W to 32W
STRIKELENGTH(meters)
5+00 - 6+Oi
1-200
1-200
300+
11-1200
FILTER RESPONSE
l Weak to Strong
Weak
Weak
Weak to Moderate
Weak to Strong
CONDUCTIVITY
Poor
Good
Good
Moderate to. Good
ifeak to Moderate
MAGNETICS(GAMMAS)
Flanking
Yes
Yes
Yes
Spot Highs
REMARKS
This conductor is locatedon the north flank of a2-3000 gamma magnetic tren(sulphide IF?)
A 5500 gamma magneticanomaly is coincident withthis short conductor.
This conductor lies alongthe same magnetic trend asdescribed in "B".
A very complex series ofmag trends which may or majnot represent a fold sincethe trends seem to be con verging at line 31W,6*OOS.-The high values point to amagnetite type IF. Two oldtrenches were found overthe conductors on line 3^W.
VLF response has been en hanced by a swamp system thowever a mag dipole .onlines 27W and 28W wouldwarrent futher attention;
MAP
If
-
k
k
if
if
f
F, G
H
I
J
K
LOCATION
19W to 2*fW5+50-7+503
19W7+oos
*
19W-22W
20W-23W
16W
STRIKELENGTH(meters)
5-600
,
1-200
300+
3-*K)0
100
FILTER RESPONSE
c
Strong
.
Moderate
Moderate to Stror
Moderate to Stror
Moderate
CONDUCTIVITY
Weak to -v -Moderate
Poor
g Poor
g Good to Mod erate
Moderate
MAGNETICS(GAMMAS)
Spot High
SlightHigh 500
None
Spot High
None - '
REMARKS
Generally there is noreal good mag correla tion along this conduc tor except on line 19 Waround 5+00 S. (3000 )The point could be madethat one could include "G"in "F" and leave the re sponse on line 19 W, 5 Sas a solitary conductor.However i without furtherinformation on thestructure in the area itwould be impossible to say.This area would warrentfurther exploration.
Minor high of 1000around the strong VLFconductor on Line 21W10+OOS
Possible the same trendas "G".
MAP
4
4
4
4
4
4
4
9
L
M
N
0
P
Q
R
LOCATION
19W- 20 W 5+50S
22W 6+OOS
24W- 27W 0+75S-0+50N
31W - 33W 0+75N
30W 2+50N
26W 3+OON
24W- 25W 5-t-OON
STRIKE LENGTH
(meters)
2-300
1-200
3-400
2-300
1-200
4-500
1-200
FILTER RESPONSE
Moderate to Stron
Strong
Strong
Strong
Strong
Moderate to Stroi
Strong
CONDUCTIVITY
g Poor
Moderate
Good to Moderate
Poor to Moderate
\
Moderate
g Poor
Poor
MAGNETICS (GAMMAS)
Minor
Yes
Yes
Yes
Yes
Flanking
Yes "
REMARKS
Minor low of 950 gammas on Line 19W
Still's eye mag of 9000 gammas over this strong conductor
3600 gammas Maf with a strong VLF response (sulphide iron formation)
A mag high of 4-7000 gammas associated with this anomaly is probably due to a Magnetite I. F.
Straddles a dipole pos sibly due to a sulphide iron formation
ill defined mag trend to the south of conductor. VLF enhanced by swamp topography
Flanking a 3-4000 gamma , high to the north. Sulphide I. F.
MAP
If
k
fc
/;
s, s*
T
u,v
LOCATION
18W- 20W 1W50N-5+50N
25W- 26W 5+50N
27W- 3^W
t
STRIKELENGTH
(meters)
3-*K)0
2-300
700-*-
FILTER RESPONSE
Strong
Strong
Strong
CONDUCTIVITY
Poor to Moderate
Good to Moderate
Good to Moderate
.
MAGNETICS(GAMMAS)
Spot High
Yes
Yes
, *
REMARKS
These two conductors are likely part of the same trend. Mag correlationon lines 20N and 18W.Sulphide I. F.
Flanking 3000 gamma dipole' Sulphide I. F.
Well defined nag trend (5-9000 gammas) coinci dent with VLF. (Mag netite I. F.) "V" prob ably displaced part of"U".
-
- 8 -
SECTION 4
GEOLOGICAL SURVEY
The aforesaid grid was mapped and prospected during the spring, summer and early fall period of 1984 at a scale of 1:2500.
REGIONAL GEOLOGY
The Bennett Lake Property occurs in the Wabigoon Subprovince and is located north of the Quetico fault. The area consists mainly of metavolcanic and metasediments that are situated south of the Hillyer Creek Dome and north of the "Seine Series" metasediments.
The regional strike tends approximately in an east-west direction and dips steeply to the south or vertical.
PROPERTY GEOLOGY
The area mapped on the Bennett Lake property during the 1984 field season corresponds withlines 16 -f OOW through 34 + OOW inclusive. Generally speaking, the geology is quite variable and changes in lithology occur quite abruptly on the property.
The legend insert on the next page outlines the geological units mapped and these in turn will be discussed in the order as they appear on the legend.
MAFIC VOLCANICS:
Mafic Volcanics comprise the most abundant rock type on the property. Most mafic volcanics on the property appear to be undefined and are massive to weakly foliated. Grain size varies from an ash (finegrained) to a more tuffaceous (medium grained) rock type. Some areas within this rock type contain quartz carbonate stringers. Although these areas are relatively scant it is of importance to note their relative location close to contacts (I.e. L-19 * OOW near baseline extending north).
INTERMEDIATE VOLCANICS:
There appears to be two distinct and easily recognizable intermediate volcanic lithologies. The first type of intermediate volcanic unit is a
- 9 -
discontinuous and interfingered lithology that Is mainly comprised of tuffa ceous volcanics. Structurally they appear in lenses that are stringy and thin with a fine to medium grained texture. Foliated to weakly foliated these intermediate volcanics are conformable to other geological units. In some instances these units may actually be an intermediate tending nore towards a mafic rather than a true intermediate rock type. However, for better geological definition and mapping identification these have been defined as a separate lithology.
The second intermediate lithology is physically significant by virtue of the fact that opalecent bluequartz-eyes are recognized in an Intermediate tuff. Also within this lithology one may observe a quartz-feldspar porphyry with and without quartz-eyes. The most prominent area with these lithologies displayed, occurs along the baseline from 19 * OOW to 27 * OOH. This litho- logical unit is quite large in size extending roughly to 2 -i- SON and 0 + 75 South.
FELSIC VOLCANICS:
Felsic volcanics on the property generally appear as small and discontinuous bands, south of the baseline. These tuffs to crystal tuffs are generally fine to medium grained and contain a great deal of silicifi cation. Banding within the crystal tuffs is quite common with most felsics revelling foliation. These volcanics are conformable and quite similar in size and structure to some Intermediate volcanics with which they are often associated.
To the north of the property larger stratabound flesic volcanic bands appear. They are thicker and more continuous. These are interbanded/bedded with sediments, mafic and intermediate volcanics. Although they are more abundant than felsic in the southern portion of the property they are similar rock types in terms of structure and grain size.
METASEDIMENTS:
Sediments are found in two distinct segments of the property. To the north of the property, sediments are interlayered with felsic volcanics, iron formations and mafic volcanics. These lithologies are approximately 25 meters in width and are thinly laminated wackes and siltstones. These fine grained sediments are lenses that are discontinuous along strike. Some segments display quartz veining and oxidation.
The second area of sedimentary deposition is an extremely broad zone to the south and west portion of the property. This may represent the end of a sedimentary unit that may be pinching out. Alternatively, this may be a large sedimentary unit that has been interfingered with volcanics.
The unit consist of alternatively bands of wacke, siltstone and argillite. The intercalated fine grain metasediments are in some zones contorted and carbonatized. These metasediments lie conformable to regional
. * ' - 10 -
striked There are, however, a series of unique folds that may be important for structural consideration south of the baseline on lines 33 +OOW to 29 * OOW( related to the sedimentary and volcanic contact). The sediments although stratagraphically significant in size have not as yet proved significant in economic terms (i.e. gold results).
BANDED IRON FORMATIONS:
The Banded Iron Formations as typically expected occur within meta sediment s. These cherty units contain varying amounts of sulphides and are associated with oxidation weathering. These relatively thin units (i.e. 1/2 meter -10 meters) in width are discontinuous and conformable with other geological units. The economic significance of these iron formations has yet to be determined, however, economic values have been attained in the ' trenched areas close to what is believed to be an iron formation. Therefore, there may be a relationship that drilling can confirm.
FELSIC DYKE ROCK:
A unique felsic dyke that cross cuts strike and intrudes country rock south of the baseline (i.e. 5 * OOS) between lines'29 + OON to 31 -l- OOH. This dyke is massive to weakly foliated and contains sulphide mineralization. Assays are not encouraging.
STRUCTURE:
The Bennett Lake property is generally massive-foliated and is steeply dipping to the south. Little identifiable faulting occurs throughout the property, however, a fault is evident at line 19 * OOW north of the base line. Trenching at line 25 * OOW was shown there is a possible faul oriented in a north-south direction. Evidence for this comes from the offset shown in the detailed geophysics.
SUMMARY:
1. The complexity of geology on the property related to a variety of litho- logical units and abrupt changes in geology over small distances, suggests that important details related to economic mineralization may have been missed by this survey.
2. This geological survey has outlined geological units that could aid in the prospecting of the property.
- li -
SECTION 5
TRENCHING
A soil geochemical survey .completed in the 1983 field season revelled an extremely high sample result (i.e. 0.05 oz.ton/Au) at location 25 * OOW, O * 25N. Follow-up prospecting (in 1984) lead to a major trenching effort just south of this location (baseline) which resulted in a showing' with extremely high values (see trench plan). The economic significance of this zone is yet undetermined, however, the geological environment has been established as a unique setting.
A highly weathered ("latheritized") iron formation of significant width (i.e. 10 meters) was uncovered with the aid of a bulldozer and backhoe. Bedrock within this zone was not detected to a depth of approximately 15 feet. High gold and silver values were sampled at the contact between banded sediments and mafic volcanics (i.e. wall rock). Within the wallrock, quartz veins and sulphides plus, telluride mineralization are identified. This zone is coupled with a good magnetic response indicative of magnetite. A strong VLF-EM conductor couples the magnetic anomaly and* is thought to be a response to sulphide and possibly pyrrhotite mineralization.
In addition to high gold and silver values a unique occurrance of native tellurium and altaite were uncovered. These minerals were identified using , x-ray diffraction methods for mineral determination conducted at the University of Toronto's, mining laboratory.
- 12 -
SECTION 6
GEOCHEMICAL SURVEYS
A soil geochemistry survey and an organic (humus) geochemical survey have been completed on the Bennett Lake property.
Samples were taken,where possable/at 25m intervals on grid lines spaced at 100m.It was endeavoured to collect soil samples at each station,however, because of abundant low-lying often swampy ground,and an erratically developed soil profile,soil was not always available.At stations with no soil develop ment, organic (humus) samples were collected.
Sampling was attempted at 2175 grid stations.From this 880 soil samples (42.9*) and 1172 humus samples (57.1*) were collected.A combined sample coverage of 94.3* was realized.
SOIL SURVEY
Soil samples were collected at stations with a developed soil profile.The B-horizon was the sampled horizon.Samples were collected with a grub hoe and stored in kraft soil bags.Each bag was marked with the line number and station of the sample site
The soil profile is locally well developed but is generally poorly devel oped to absent.The B-horizon usually occurs beneath 2"-18" of lcached,puggy, grey,Al-horizon soil.The B-horizon is often rocky,probably often being glacial till cover.
All soil samples were analyzed at Technical Service Laboratories, Mississauga,Ontario.All samples were analyzed for gold, zinc and copper.
Values for each element are plotted on the accompanying maps at a scale of 1:2500.Gold is plotted as ppb,copper and zinc are plotted as ppm.
GOLD
Values range from (5 to )1000ppb (0.04 oz/ton on check assay).The mean value and standard deviation calculated from 861 samples are 9.6ppb and 16.6 ppb respectivly.
Gold values as plotted are not amenable to contouring because of the high number of no-soil locations.Instead ,a symbol map is presented with the following divisions,
18 - 34 ppb l-2x Standard Deviation 35 - 51 ppb 2-3x Standard Deviation 52 - 85 ppb 3-5x Standard Deviation
" 1 3 "
86 - 119 ppb 5-7x Standard Deviation120 - 153 ppb 7-9x Standard Deviation154 - 187 ppb 9-llx Standard Deviation
) 187 ppb )llx Standard Deviation
Gold value are erratic,forming several areas with "bullseye" anomolies and only several anomolous "zones".Highly anomolous areas are:
L22+OOW Independance Shaft 630ppbL25+OOW 0+25N )1000ppb (0.04 oz/ton)L19+OOW 5+25S )1000ppb (0.01 oz/ton)
The west map sheet also has numerous other weaker anomolies that are being followed-up.The area west of L10+OOW has a much higher percentage bf anomolies than east of this line.
DETAILED GOLD SOIL SURVEY
A detailed gold geochemical survey with 25 meter spacing and 25 meter centres occured as a result of some high gold values in the soil (ie.see above values). The grids boundaries roughly cover L-l9 to 27W and from 1+25S to 2+OON.
Detailed soil sampling for gold, resulted in erratic values ranging from n.d. to 464ppb. No significant zones and or halo effects can be interpreted from the gold values,in soils.
COPPER-ZINC
Two copperXzinc anomoly were detected during the course of the survey. Locations are as follows:
Zn Cu Au
L25+OOW 1+75S 2400 550 120ppb L26+OOW 1+OOS 3000 425 12ppb
The data is plotted on the accompanying maps at a scale of 1:2500.
DETAIL COPPER AND ZINC SOILS
Detailed follow-up for copper and zinc on a portion of the detailed gold geochemistry grid proved more successful. The main area of concentration lies between lines 24 and 27 west and from the baseline to 2+OOS. Hithin this zone there are some interesting zinc results. Values for zinc geochemistry (ie. soils) range from 40 ppm to 3000 ppm. Copper values roughly couple with zinc values in two zones. Copper values range from 8 ppm to 1350 ppm. A
- 14 -
diamond^Orill hole (BL-4-84) tested the copper and zinc anomalies on line 25 west. Drill core from this hole shows calcopyrite and sphalerite.
ORGANIC SURVEY
Humus samples were taken at stations with poor to no-soil development. Samples of decayed or decaying "forest litter" were collected by "scooping" with a grub hoe or hand.Samples were taken from the A-horizon immediately below actively growing vegetation.
All samples were analyzed for gold by the neutron activation method at Nuclear Activation Services Limited,Hamilton,Ontario.
Gold values range from Oppb to lOOOppb.The mean and standard deviation calculated from 1037 samples are 2.9ppb and 4.6ppb respectively.
Data is plotted at a scale of 1:2500 on the accompanying maps.Results are presented as a symbol map in the same manner as for the gold-soil survey with divisions at :
6-10 ppb l-2x Standard Deviation 11-15 ppb 2-3x Standard Deviation 16-25 ppb 3-5x Standard Deviation 26 - 35 ppb 5-7x Standard Deviation 36 - 45 ppb 7-9x Standard Deviation 46 - 55 ppb 9-llx Standard Deviation
)55 ppb )llx Standard DeviationGold values are erratic with several strong "bullseye" anomolies.The
strongest anomolies occur at:
L31+OOW 10+25S lOOOppb L20+OOW 2+OON 620ppb
Most anomolies occur on the west grid sheet with no anomolies occuring east of L10+OOE.
. - 15 -
SECTION 7
DIAMOND DRILLING
To the west end of the Bennett lake property, four drill holes were drilled in December of 1984. All four holes were collared on claim f676196. Enclosed within this report are copies of the drill record, longitudinal sections and assay results.
Holes number one and two were drilled to test a coincedent mag. and VLF anomaly. Drill hole BL-1-84 was 328 feet long and collared at L24+92W/0+35S. The drill hole in addition to testing a mag and VLF anomaly also tested a gold and tellurium showing on surface adjacent to a highly weathered and trenched zone. A vertical projections from down the hole to surface suggest this weathered zone consisted originally of massive sulphides (le.pyrite, pyrhotite,sphalerite). Assay results from these two holes where considered anomalous although no ore-grades were encountered.
Thcobjective of the third drill hole (BL-3-84) collared at L22+08W/0+24S was designed to test the old mine shaft. The hole was drilled to a depth of 253 feet and results from this hole were less than encouraging with quartz veins displaying an extremely bullish tendancy. Results from through out the shaft area (le.adjacent rock,mine dump,drill hole ect.) have not given any evidence for the justification of the Independance mine.
The fourth hole drilled (BL-4-84) was drilled to test a gold/zinc soil anomalies plus, test a mag. and VLF geophysical anomalies. This hole was collared at L24+85W/2+10S. Results for this 293 foot hole, were not good however, sulphides including pyrite,pyrhotite and sphalerite were encountered in the core.
- 16 -
SECTION 8
CONCLUSIONS
1.) Proton Precession Magnetometer and VLF Electromagnetic surveys were successful in defining potential zones of mineralization for follow-up exploration.
2.) The trenching program that occurred in the latter part of the summer established a good gold showing with economic values on surface. Furthermore, a unique assemblage of minerals were identified including native telurium and altaite (gold-silver-lead teluride). However, drilling failed to confirm the showing at depth but, there is still a need to determine the structural and genetic aspects of the showing. The Royal Ontario Museum's Department of Earth Sciences has expressed interest in looking at this showing and possibly spending a period of time this upcoming summer working on this area.
3.) Geological mapping on this property, although simplisitcally shown on the maps provided is much more complex. Abrupt changes in llthological units over small distances occurr within some areas. These changes may have resulted in possible mineralized zones being overlooked during mapping procedures. The mapping program has outlined areas that are worthy of prospecting .
4.) Although no significant results were attained from the drill program under taken in the late fall, anomalous values up to 0.12 oz/ton were encountered. There are still anomalies that have not been tested that warrant further investigation.
.. fT 17 -
SECTION 9
REFERENCES
1.) Ontario Department of Mines, Volumes 1899,1900,1902.2.) Ontario Department of Mines, Young 1960.3.) Ontario Department of Mines, Fumerton 1981.4.) M.R.C. No. 13, Ferguson et al, 1971.5.) Resident Geologists Files, Kenora and Thunderbay.
Map References:l2.3.4.5.
Map 2443 Kenora-Fort-Frances Sheet ( Blackburn,1973-78)Map P2405 Calm Lake AreaAeromagnetic map 11426O.D.M. Geological Compilation Map 2115Map 190b Bennett-Tanner Area{Young 1960).
Submitted by:
Peter Mordaunt
Randy Crowley
LYNXCflNflDfl EXPLORflTIONS UMITED
DIAMOND DRILL RECORD Hole No- One
Hou M* 1 Ri^t ' 1
To*n.hlp L 24 4- 92V 7 0 * 35SLocation
f— ̂ ,,ft fMl.Bmrinr 330 d*pra*c|)|p — Srt HocrrAosObjertivn iO tvat tvllnrium anH
"lafpritir^d" trenchar**a
Complttai DacAobfli* \ l "8'irMiiinff na. UorwesconCorf Size — ̂ - B QCaning Left ip Hota . ... f f^ct
R^.A,
.1 Footage1 From
1 21,5
1 72.5
LN-
To
21.5
72.5
96.5
Dip: (
Etch 1
'^i.r - 50*Test Depth Rdg. True
150 ft. 53 44 0328 ft. 50 41*
DESCRIPTION
Mafic Volcanic that if hiehlv oxidized with chlorite alteration nlus rmartK vAininoand stringers^. biotite mineral i xa t inn On fracture nlanes vith leaa than l? Hi ASA—O^Hv.ed sulphides fnvrite}
Intermediate volcanic tuff with MJUA miai-t* AVAO. nuai-t* oM-inoora fmillrv wfcitA^
Intermediate -and bands of i
- Felsic volcanic vith mtl phi den•ica and sericite O— 5 imn^ -
Sample No.
10601
infin?1060310604106051060610607106081060910*10infillinfii?infin
From
12
72.575777981838587RO010?QS
To
13
757779ft18385
89Ql93
Oft S
Length
1 ft
2 ft2 ft2 ft2 ft2 ft2 ft.2 ft.2 ft? ff.7 ft? ft.IS f
Location Sketch Nort
Clain
Scale
Au ppb
5
* 531
g35
< 531
5485
17121
HO346
*\K—. .-...j. **pp^H
1.0
0.60.7O 91.70.91.48.21.14.11.43.67.1
Zn ppm
tt,
i
i
P* . r
1" — 10WV
—— —————— L— ——— ' ———
LYNXCflNflDfl EXPlORflTIONS UMITED
DIAMOND DRILL RECORD Hole No- Sheet No.
DH -
Foot)?Vom
56.5
115
m
148
151
174.5
178
L'\
**eTo
115
134
148
151
174.5
178
.183
E* O O ft 1 r 1 I i/ W
TnffrrniPdiflt-A t-itff wii-l^ cfy^tch^J blue quartci cyeo'lcoo than 11 atilnhidea
Banded intermediate - felsic volcanic with chlorite, sulphides (up to 102). quartzveins and stringers, micaceous segments that are banded: micro folding with bands
Intermediate - Mafic volcanic with blue quartz eves, less li suluhide mineralizatio
Chloritized contact between Intermediate volcanic and Intermediate - fei air-volcanic (rich in sulphides).
-Intermediate - felsic volcanic with bands of chlorite, biotite and mil phi den upto 20Z, some quartz stringers and possible sericite alteration.
MASSIVE SULPHIDES
.Sulfide Iron .formation-- (py,-po, opy) possible magnetite, chlorite rich band* with relic felsic- intermediate volcanic
SampleNo.
1061410615106161061710618
1061910620106211062210623106241062510626
1.1062
1062810644106291063010631106321063310645106341063?10636
10637106381063910640.J 0641
from
9fi S.99102105114
115118121123125128130
134
151153156159165168171162174.5176177
17ft179IflO-181182
10
QQ102105108115
11812112312512813031.5
38
15315615916216817174.5165176177178
179.180181182 -1 01
Ltncth
' ** f t3 ft.3 ft.3 ft.1 ft.
3 ft.3 ft.2 ft.2 ft.3 ft.fe ft.-S
2 ft.
l ft.
2 ft.3 ft.3 ft.3 ft.3 ft.3 ft.3.5 f2 ft.1.5 f1 ft,1 ft.
1 ft.1 ft.1 fti.-f-ti-i ft.
Auppb
SA^ s< 54. 5< 5
275721131230liT70
13
327306119131
8101
. 123IfiSl-.. 10
13< S
113276ftSI?Aft
-.2572.
Agppm
1.0n 70.60.60.9
1.11.30.1
^0.1^0.1^.10,60.2
XQ.l
3.9CQtl0.91.61.53.20.64.30^80.70.5
3.171i.n0.31 ̂
Znppm
0.054
0.033
O.O7S
oz/ton
oz/tor
Au
Au
Au
LYNXCflNADfl EXPLORflTIONS LIMITED
DIAMOND DRILL RECORD Hole Sheet No-
M, PH - l - 84
FootiProm
-J83
185
193.5
208
228
233.5
if*To
185
193.5
208
22ft
233.5
251.5
boV/Klrl 1 U PI
Sulphide Iron Formation (massive sulphide)
Sulphide Iron Formation with up to 35Z sulphides (py, ppj cpy) , alteration bandsof chlorite and biotite plus magnetite
Banded felsic — Intermedia t- e volcanic with sulphides up t-o 302, po t py.
blup qua rt x f yea , —————————————————————————————————————————————————Contact zone that Tft hivhlv alt**r^*]l to ohlo^it* arid hiotitfe adiacent to sulotiides
Sulphide Iron Formation .po t py^ in addition hands of chlorite and biotite-alteration, massive sulphides in segments
f
SampleNo.
1064210643
1064610647106481064910650
.lOfiiL1065210653
10654106511Q65A1Q65J.106*18lOfiSQJjQMD.infifiiinfiM
lOfifil10676lOMi.ipees1066610667JLOfifift.1QM2.106701067110672106731062410675
WMMA
183184
185186187188189190191192
193.519519719920120520420S207
21A*3-230231
233.5235237238239240241.5243244245.246
To
184185
186197188189190191192
193.5
1951971992012032042(tt20720ft
.221231233
235237238-.239240
141.524324424 S
.246 .247
Length
1 ft1 ft.
1 ft.1 ft.1 ft.1 ft.1 ft.1 ft.1 ft,1.5 f
1.5 ft2 ft.2 ft.2 ft.2 ft.1 fi-.1 ft.2 fi-1 ft.
2.5 f1 ft.2-fJ^
1.5 fi fit*.1 ft.1 ft.1 ft...5 ft.5 ft1 ft.1 ft.lit*.1 ft
Auppb
79180
370106
50180
18863841
800123
11850
106165454580'Ut
270
532697
-31116168
—2M.29211616022413264
, 56.
kgppm
^0.1< 0.1
3.04.22.60.8
14.224.422.98.1
8.2*:o.i
3.20.1
* 0.1< 0.1< 0 .1-o-
1.2
^.6.10.6
*C0.1
0.61.1
.JiiA1.22.71.10.11.33.61.2
.-4.JL
C.TLppm
0.0550.112
OZ/tO!
OZ/tOI
•^•MMP^tfMB
"SAu
Au
LYNX-CANBDfl EXPLORHTIONS UMITED
DIAMOND DRILL RECORD Hole No. DH - l - 844Sheet No-
FootFVom
251.5
' 260.5
262
268
295
**eTo
260.5
262
263
295
328
lv d is K 1 * 1 1 w FI
rnNTTNTtim
Intermediate - Mafic volcanic with bands of chlorite and sulphides uo to 52. bluequartz eyes, quartz stringers
*
Sulphide Iron Formation (massive sulphides)
Intermediate - Volcanic with disseminated sulphides up to 5Z, - zone of 60Z po(266-267) + cpy less 1Z
Intermediate volcanic with small stretch blue Quartz eves. disseminated sulphidesup to 5Z
Intermediate - Felsic volcanic banded sulohides (15Z) with auartz stringers andblue quartz eves.
END OF BOLE 326'
————————————— i —————————————————————————— -. ———————————————————————————————— : —————————
SampleNo.
0677067806.790680
L0681L0682L0683
L0684
10685L0686L0687LQ68810689L0690
106911069210693106941069510636.10697
10698106991070010520IQ52L-10522-1052310524.10525
TTvfn
247248249250
251.5254257
260.5
262264265.5267268270
273277280283286289292
295128.301207310313316119121.
10
248249250
251.5
254257
260.5
262
264265.5267268270273
277280283286289292295
298301 .307310313316319121324 .
Length
1 ft.1 ft.1 ft.1.5 f
2.5 ft3 ft.3.5 ft
1.5 ft
2 ft.1.5 ft1.5 ft1 ft.2 ft.3 ft.
4 ft.3 ft.3 ft.ft.
3 ft.3 ft.3 ft.
l-fJl..3 ft.6 ft.3 ft.3 ft.3 ft.3 ft.5 ft.4 ft.
uppb9688
12352606
. 47155
1440
. 580
411097
. 352216022983
7611478871912025
121219754ft49361518
^ 5
ASppm
2.:2.:8.126
4. C< 0.1
4.1
3.(
0.43.1.1
12. c2.!0 '1
< o .^ Q-C 0.1ai — yjL—t 0 .1
0.9o.:0.!
0.42.?3.31.7
^ o t0.60.
^ 0.0.4
Znppm
0.0360.076
0.042
0.032
0.063
1
OZ/tOIoz/tot
02 7 tOI
OZ/tOI
oz/tot
'
.Av .Au
.4v
Au
Au
LYNX-CflNflDfl EXPLORATIONS LIMITED
DIAMOND DRILL RECORD Hole No. BL - 2 -(
HA!* No RT.2-R& |t^— t 1 Of 6Property Rennetfc LakeTnw^ihip Bennett TownshipLmtbiii
L25 4- 16W0 4- 60S
l*^..^.
r— tfk 400 feetItarinr 330*r*r -50*OVHtiy
Test Mae 4VLF-EM Anomaly
Commeimd Pec ̂ 3 p 1984n^pi^i Dec. 5. 1984Tvflti"jr o Norwesconr™, si— B. Q.r.rfnfl i*ft in H*if 7 feet
FootageFrom
0
7
87
111.
111.
To7
87
111
1 111.3
J 128.0
Dip: (VII., -5- 0 iU)catioa Sketch
Etch Test Depth Rdff. True
400' 48" 39"
DESCRIPTION
Casing Overburden .
Intermediate Volcanic Rock- Blue Quartz eves- Surface weathering to 21 feet. Blockv Core
13 '-23* 4 feet of eround core23 '-24' bands of sulphides 1 mm thick24 '-42' 1Z disseminated pvrite63 *-87* sulfide*: are coarser arained dissemination with less stringers sulphide
87-88.5 sphalerite in narrow strineers with minor pvrite
Altered chlorite zone- contact zone to sulfide zone below
Massive sulphide band - nvrite
Intermediate volcanic rock ^.- blue Quartz eves
fine erained at ton of section coarsening down the hole f ran 1 25. O - 12R.Or Well banded sections r handing defined hy thin hands of nvrit-0 2 mm. Also
there is a conroositional handinf -. quartz. rich and enidnt* rhorite hand*Also nvrite occurs as fe. disseminated and a Imur fracture nlanon uirhchlorite.
Sample No.
105261052710528105291054010530
1053210533105341053510536
1053710538
10539
10^-310-55410SV5
From
108
23273237
6368737883
8788.5
110 5
113ria123
To
139
27323742
6873788387
88.593.0
111.5
118
12ft
Length
3145'5'5'
5*5 f5*5'5'
1.54.5
1.0
5'
51
.
Aft*
1976
1176
11^ 5^ 5
1315
11< 5
"8ft
11li
6
North
1Claim 1
Scale:
ppmQ. 5
*C 0.10.10.1
( 0 .10.3
0.20.10.20.40.4
0.5Q.s
"2.0
1,3fi. 50.3
Zn ppm
*
460
40702110
225
0.40Z0.21Z
No. -..,,..
*— XW1
ZnZn
)'
LYNX-CANADfl EXPLORflTIONS LIMITED
DIAMOND DRILL RECORD Hole No- Sheet No.
BL - 2 -
FootSVom111. J
128'"
139.5
ttl.'S
1C*To128.0
139.5
141.5
153.0
bov/tllrl tvn
Continued
123-124.5 4 quartz bands - 1 cm each no Sulphides in quartz.but there is e.g. disseminated pyrite in the tuff.
Quartz/Sulphide Zone
Zones v 1 foot of massive sulphides rich in quartz within a quartz eyevolcanic
*
Massive Sulphide 7nT^eg — llf— 7 — fjy 5 pyritfl135.5 - 136.5 nvrite
Sulphide Rich Zones - 133.0 - 134.2 py-qtz 20Z138.0 - 139.0 py-qtz. 3.4Z
* Pyrrhotite occurs aa v.f.g. dinneminflM'ona-locally throughout ZDne ( lint not in t-tte maeaiva a*ftinna
Intermediate Volcanic- blue quartz eyes- lr-2Z disseminated pvrit* and pyrrhotite
Chloritic Volcanics- massive r minor ovrite and pyrrhotite ^ liminor pyrite bands neat bottom of zoneDiffuse contact over 1 foot -t hntt-nmSharp uooer contact.
SampleNo.
10541105421054*
mss*10557iPJLHL1055Q
PMdkBM
t2R133137
lil158163
IfiS.-i
W*-10
133137142
158163
165.5lfifi.1
Length
5'A'S'
s5
2.4.fi
kuppb
3230458
33411797
Aefjpm
1.111.8
(C 0.1
0.31.0o.?1,2
Znppn
LYNX-CflNfiDfl EXPLORATIONS LIMITED
DIAMOND DRILL RECORD Hole No- Sheet No.
BL - 2 -,
VbotiFi*.
-. . 153
172.0
177.7
L^
igeTo
172 r Q
177.7
202.0
D C*Cf*DIlft^ffS\lkJb D l* K 1 r 1 1UN
Silicic - qiue quartz eye volcanics ——
165.5 - 166.1 chlorite rich zone as above
disseminated and banded sulphides CA fiOtprimary sulphide bands 2 mmsecondary pyrite in discordant bands and stringers and qt* veinsOverall 1-2Z pyrite with zones up to 5ZGradational lower contact.
Magnetite - Porphyritic Zone- rounded crystals of magnetite ^ 1 mm
in a chloritic and epidotized volcanic (?1Magnetite by volume is 2-5ZSharp contact with underlying sulphide zone.
Massive Sulphide Zoner e.g. crystalline sulphide (pyr i l-*) Bn^
Quartz (clear ervatall in* V- 70-90 I aulphiH*
J77.7 - 195.0 Pyrtt* Zftn* v*sty mi'nrvr pjrr^nfil-azones with minor mametite
195,0 - 202.0 Pyrite, pyrrhotite Po content increasesdown in section until Po-70It of th** mil phi daMinor chlorite throughout.
SampleNo.
insfin1056 L1054410545
ins&fi
10S47lOSAft1054910550inssi
VUuhM.
Ififi 1
IfiQ172. C173. C
T75.5
17fl1A418ft19310ft
•p*
169j 7? n173.0175.5
178
183t Aft191198901
Length
7.93.01.02.5
2.5
.5 ——5 'S *s
-5 ——
AuPPb
2fi^79
2015
68
9893317RB5
Agppm
^n i0.50.50.1
0.7
1.00.60.9(Kft1.4
Inppm
'
LYNX-CANflDft EXPLORATIONS LIMITED
DIAMOND DRILL RECORD Hole No- Sheet No.
BL - 2 - 844
FootiFrom202
205.5
f*To205.5
328.0
CiOlyKlrllUM
Pyrrhotite — chalcopyrite zoneChloritic with semi massive zone of po with cpy. Sulphide occurs asStringers. Host rock is rhlnr-i t-ir and si 1 i rpniifi UA! 1 Vian^ad fuf f /vnl rani r2" - 3" hanHs nf SO2 po wi'Hi ^ ?T npy
Quartz - porphyritic crystal tuff
- Variable unit, from barren massive tuff to very well bedded tuff-sediment
- siliceous with zones of quartz veining and brecciation
- sulphide is mostly py f with lesser posulphide occurs as conformable stratigraphic beetsof sulphide to v.f.g. disseminations in hostrock and as coarser grained pyrite inquartz veins.
- garnet, porphyroblast s 1-2 mm inExtensive quartz ve in in R from 206-0-215.0 minor pyriteat 214. It is more abundant in the host thanveins .216.5-223.0 minor nvrite in Quartz veins mo s t lv in host.
228.0-229.0 e.g. py-pn within quar f r v*in 1OZ sit 1 phi Ho238.0-243.0 infenae quartz veining - VAJTI hraoria
SampleNo.
10552
10562105631056410565105661056710568iiooy105701057110512.105731057410575105761Q577JLQSJfl.10579iom1Q28X1Q5W
PtatlitMrrotn
203
206210215220223228233238253257264277279283288^93298303308313918
T*10
20fi
21021522022322823023824325726026527928328829329ft303308313114.. *)123
Length
3 0
45535255431245^55551.55,0
Auppb70
1117595461
2784323235?6
77*U8999
20576
30< 5
Agppm1.8
< 0.10,10.30.10.52.8
( 0.10.1
< 0.10.4
< 0.11.6
10.42.50.80.30.91.2o.i0.20,3
znppm
42
LYNX-CflNfiDfl EXPLORATIONS UMITED
DIAMOND DRILL RECORD Hole Mff BL-- 2 -l Sheet No 5
FootiProm205.5
328
iceTo328.0
400'
baCKlrllUN
continued
253.0 - 260.0 very well bedded zone with f .g. minor quarz veining
264-265 white quartz vein, chlorite garnet277-279.0 sphalerite in narrow stringers 2mm wide running parallel to core
for 2'279-283.0 well banded pyrite in well banded sediments. ^ 6Z in places
*
288-293.0 very well banded sediment - tuff withstratiform pyrite bands289-290 51 py
314.5 - 328.0 gradtional zone into unit below increasing amounts ofchlorite and biotite
318-328 quartz veining in chloritic tuff some epidote.
Mafic Volcanic Rock
- chloritic and biotite rich- biotite defines a crude foliation 30" to core axis- numerous quartz and quartz carbonate veins i. 2" wide.- gradational and alternating contact with above unit to 331.0V
341-343 quartz -carbonite - chlorite biotite zone1SS-1S7 ~ ~
END OF HOLE 400*
SampleNo.
11
r rom To LenfthAu t.
ppbAgppm
-
Znppm
LYNXCflNflDfl EXPLORATIONS LIMITED
DIAMOND DRILL RECORD Hole No-
Hole No. —3-,.,.., .,,,,M, , . Sheet —— 1 —————
"^Wnihlp fifiDQfitti T-akfIMH,~, L22 * 08W/0 4- 24S
i .uii 2 S ̂ 'p^B . 5oO"-, —sn 0Pjp . ?"QKjj^tf.f Td test old mine shaft
Coniinvficfed uDfiC.a. "g 1Q8&r^pw^i Dec. 12, 1984Drilling- Co. Norwescon
'a f\Gor* Sil* ' ViCuing- I*ft fn Hoi. 3 feet
R-m--k-
FootageFrom
3
51
'X
To51
253
Dip: Coll
Etch Ted
.T -50"
t Depth Rdg. True 250 50* 41*
D E SG R I P T I O N
Intermediate volcanic wit-h Mn* nnav*-* *woo f™oT,i,r f^Ha*-,,^- 5.5" quartz Stringer with 2Z ovrite mineral i K*tion'- 10.5' 2" quartz strineer (bullish)~ 20-21' Quartz stringer with 2Z snlphid* min*fali*at- inn- 24-25' quartz vein 4" wide with less than l i .ulnhid..- 32-37 well banded zone with handed an/1 A i o a e'minatAri cnlph-Mog yp fO 2J (pyrita)
banded intern- 51-56* f. R- 63-65' f. g
^di ate vol c an i c tH t-K fc 1 KA q,i*^*- * ayes —————————————————————
. disseminated sulphides less than 1Z- 68-71* 2 qtiavt-x vein a hnt-li t 1 /9*' ^iAa SX..1 1 1' c,V.t" 74' 2 zone : : or band of chlorite-.77-80' disseminated sulphides less than 1Z~ Bo** Si * zone of banded sulphides UP to 2Z oltis a 3'* Quartz vein.
- yi-y*' quartz vein with sulphides up to 1Z plus Coz-- d^-lui 1 quartz vein with 1Z sulphides- 128-128.5* band of chlorite- 142.5-144 band of chlorite- 151-154 well banded volcanics with chlorite and hint-it-n
bands of alteration plus bands of quartz veinlets and sulphidesup Co 31- 188-iyU banding as above. —————————————
- 195 - well banded volcanics with band* of c*.....aiilpKid* f frt W
llnritfj hinM'fo, qiiarl-r and ———
Sample No.
1058Q10590105911059210593
Jfl2t610595105961059789148915
10598105998916
1060089178918891989208901890289031J9041905
From
S10192332
SI636877738286919599
10410911411913014014515?169
To
to13212637
__ 56.6873827786919599
10A109114"9124135145148157173
Length
53335
——, 5-55544554555555534
Location Sketch North
1Claim ]
Scale:
Au ppb345
26392316
s2630
101< 5540
2665
421316181220
53823
ppm^. i{ l^•1^ 1
-l
^.1l 1^.1^.^ t^.^.^.^ .^^,^^( .^.1^ .1^.^.<
Zn ppm
Parent
111 M 4AAJy
LYNX-CflNflDfl EXPLORATIONS UMITED
DIAMOND DRILL RECORD Hale No-. Sheet No.
— FootiFrom
teeTo
D vafn t DTf^u
- 208' quartz 'vein - to core axis J ' * wide
SampleNo.
89068907890?89098910891189128921
h-
IXij- win
176185195207219230240200
1**
17918ft199209
2215235244202
Length
3342
2.5V4'2'
Auoob
230555s
107^S
AuDDffl
^.1^.1*.l< ,1<.l< ,1^ 1< 1
Znppm
.
LYNX-CANflDfl EXPLORATIONS UMITED
DIAMOND DRILL RECORD Hole No.
HnU M^, ,.4 ,, Sh**t 1Piropwty JieiU) e 1 1 LakeTnwnfVip Bennett LakeI^a- L^f + ftrW
2. -H o S"
KM..*.
Length . 2Q3 Comtntnffd . J?er- '^ ( 1Q8A riip- C""*"" ** ^^Bearing 360 Completed Da c 17 1984n.p " -50* ivntWc- Norwescon Etch 1Objertir* tQ test soil r r iii Orp fFirr B Q ^
Test Depth Rdf. True 293 50* 41"
EM ^ MAG r..,'off f*ft fn HnU 13. feet^TIOTWA 1 1 f* fi
— FootageFrom0
"' 13
19
24
40
42
44
46
—
To13*
19
24
40
42
44
46
61
DESCRIPTION
Casing overburden
Intermediate volcanic with very fine grained stringers of milky white quartz - tofoliation, pink blebs of auartz disseminated throughout zone (less than IZ). Thesepink blebs occur throughout the hole and mav be earnets. Thev are very finegrained and are best described as blebs of pink auartz UD to 2mm in size.
Zone of auartz veining and stringers (net work) that; are brecciated in segmentsf. K. disseminated sulphides (IZ), pink quartz blebs (less than IZ)
Intermediate
Quartz veinvein
volcanic with a few verv small and venr fine grained quartz stringfjrj
1 1/2" wide with a zone of brecciation 1 foot either side of the
Same as 24-40'
Same as 40-42
Banded intermediated volcanic with, f ̂ — hand* nf-jni^ amLpkloi-i' fa , qt.ayt-*stringers throughout zone, less than IZ sulnhides fnvrite identified)"
Sample No.
8922
89238924
B925
89268927
From
19
28
40
44
4752
To
24
_ 3JL
42
475255
Length
51
V
2'
1'
5*3*
-
Location Sketch Not
Clain
Scale
Au ppb
624
^55
lOfi
7
11024
Ag ppm
i
1 -2
1
^.1
.1C.I
Zn ppm
*
tt!
l]
*
'
\
Wo, 6/6J96
B'
LYNX-CflNADfl EXPLORATIONS LIMITED
DIAMOND DRILL RECORD Hole No- Sheet No.
^ FooUceFrom
- 61
65 .
69
83
93
116
127
To65
69
83
92.5
116
127
173
DESCRIPTION
Foliated intermediate volcanic - not well Kanri*r1 aa in Afi'-fil 1
Intermediate volcanic with quartz veins and stringers brecciated. Stretched outquart* ey** *Ulro 40 '-49' and 44 '-46'
Foliated intermediated volcanic. 2' 1 quartz vein at 78' and a few 1Z pinkquartz blebs throughout majority of segments
Well banded intermediate volcanic83 '-85' - 10Z bands of pyrite in segment93 '-3" vein of milky white quartz P no sulphides
Poorly banded intermediate volcanic with less thanlZ pink quartz blebs101 '-f. g. stringers of sphalerite Q/2 mm) associated with quartz strineers
Well banded intermediate volcanic, bands of chlorite, mica and biotite alsopresent are small quartz strineers (1-2 mm) plus blebs; of pink quartz
Weaklv/poorlv banded intermediate volcanic with pink quartz blebs, segmentswith PV. PP. .oh. (Same as 93-116) ——————^.———-————————-——————-———
136' - Quartz atrineera + 3Z ovrite140 '-142' - zone of quartz stringers, po * py banded
up to 5Z sulphides144* - quartz vein up to 2" in width with po -f py associated
(uo to 2Z sulphides).152 '-153. 6* - vuffirv quartz with pyrite in bands UP to 15Z, quartz also in
ve in let a and stringer*1fiO'-1fi3* - Hift.eminated 4- banded pyr po r apRaljerite . CPV un to 15Z
Sample No:
8928
8929
89308931
89328933
89348935
8936ftQ17M388939894089419942894389448945
From
65
76
8388
93?8
116121
126.,.
1361411461511561(1166171
To
69
78
8893
98102
121126
131136141146151156161166171176
. ..... -
Lenrth
4'
2'
L5 14'
5'4'
5'S*
5*giVr5*5*5*
yr5'
.
Au ppb
5
< 1
< 1IS
2813
1131
< f9023148536
< 5275
-JA^
Ag ppm
^.1
.2
1.7I.*
.4
.2
.6• 3
• 2.2.3.3.3.Q.7
1.01 k1.5
Zn ppm
137
465120013QQ1255
LYNXCflNflDfl EXPLORATIONS LIMITED
DIAMOND DRILL RECORD Hele No— Sheet No.
Foot)Prom173
190
201.!
208
216
289.5
1(0
To190
201.5
208
216
289.5
293
bov/Klrl 1 U Pi
177 '-178* - quartz strineers banded with bands of ov + oo uo to 10?181 '-183' - quartz veins and stringers; sphalerite strineers
Weakly banded intermediate volcanic with quartz strineers and minor pyritedissemination
Zone of highly chloritized volcanics206-5 - 207.5 - quartz with pyrifs 9aenoiat*d uifh
Banded intermediate volcanic with quartz veins 4- strineers hands of sulphidesup to 20Z, chlorite banding
Poorly banded intermediate volcanic with minor ovrite mineralization, less 1Zpint quart-* h1**ha.
228 '-230' - xnne-.nf hi HP qnnrtr oy"245 - UD to 10Z oink auartz blebs269.5 - auartz vein 2 1/2" wide minor sulphides (pyrite)275 - quartz veinine over 6 f * wide section with minor- aiilphiiWpyHte 1*
mineralization
Mafic volcanic that is chlorite rich and banded with chlorite A hiotite
SampleNo.
894689478948
89*98950
8951
8952
8953895489569957958
RQSQ
8961
VvuuMrrom
17fi181186
191196
206.5
207
213218232*5.250268?r\
289
To
1R1185189
194198
207.5
213
218221232*5.253273221 ——
291
Length
S'A 13'
3'2'
1'
6'
5'3*
r3 f
Auppb135
<5
* 5< 5
17
35
17< 5S K
* l
11888
Agppm1.3.7
1.0
.6
.8
.7
.9
.6
.4
.4tA-A.9
2nppn
12501200995
218
t 52C1BSECM5 63.4MB BENNETT O2O
LYNX CANADA EXPLORATIONS
ALICE'A' PROPERTY
Submitted by: Peter Mordaunt For Lynx Canada Explorations Ltd
Qrt 02-
-1-
INTRODUCTION
The following report details the results of a major exploration effort undertaken by Lynx-Canada Explorations Limited, of Toronto. The property examined is called the Alice"A" after an occurence that is almost completely sorrounded by the claim group. The program occurred during the summer and fall of 1984.Exploration procedures consisted: of two geophysical surveys, including a proton precession magnetometer and very low frequency electro magnetic survey,a geological survey, prospecting, and a basal till sampling program. All surveys include the appropriate naps at a scale of 1:2500. Sample results from mapping prospecting and basal till sampling are also included within this report. Furthermore this is a preliminary report since additional exploration is still considered at the time.
-2-
LOCATION and ACCESS
The property is located south of the Little Turtle River In the areas of Bennett Lake (M-2392) and Little Turtle River (M-2433) In the Kenora Mining Division. The property lies 50 km. west of Atikokan/Ontario and north of highway #11. An abandoned town of Glenorchy is situated within the eastern third of the property. Access is obtainable via the Bowe's Camp road and the Martin's or Glenorchy road which intersects highway #11.The Bowe's Camp road roughly dissects the claim group in half. Access by foot along old logging roads and by boat along the Little Turtle River is possible from the above road,
PROPERTY
The Alice"A" property consists of 73 unpatented aining claims as follows:
759737-54759757-76759797-803759809762446-9762701-23
18207l4
24
73All claims are recorded in the Kenora Mining Division on plans M-2433 and
M-2392.
PREVIOUS WORK
The area of major interest is the Alice"A* prospect.Although the prospect is not within the claim group, it is sourrounded to the north, east and west. Furthermore, since the local strike trends in an east-west direction there is no doubt that the horizon containing the Alice A deposit strikes through the Lynx property.
Alice"A" History (l)
1894: The first reported trenching, sampling and surface observation was in 1894. A three foot (0.9 meter) deep trench disclosed a network of veins striking parallel to the schistose country rock. The property consisted of two mining claims K190 and K191.
1897: The property was owned and developed by the Anerican-Canadian Gold Mining Company of Nest Superior, Wisconsin, with Mr.J.S. Hillier, president and Mr.G.H. Hillier, manager. Intial work began in July,1897 and consisted of trenching across the structure with test pits approximately 10 feet (3 meter) sunk at each end.
1898: American-Canadian Gold Mining sank shafts approximately 200 feet
-3-(61 meters) apart with a number of small test pits for test purposes. Shaft No.l, 46 feet (14 meters) deep has cross-cut north 30 feet (9 meters) at a depth of 40 feet (12 meters), and shaft No. 2, 200 feet (61 meters) east of No.l,is 70 feet (21 meters) deep with a cross-cut at a depth of 60 feet (18 meters) running 19 feet (6 meters) south.
Fall 1898: One two-stamp Tremaine mill was Installed for test purpose with a 3 ton per day capacity. Approximately 150 to 200 tons of ore, taken partly from the shafts and partly from the various test pits on the property were treated. The Alice"A" Mine is reported to have been sold to an English Company under an agreement to install a large mill of 100 or more stamps. As shaft sinking continues, Shaft No. l reaches a depth of 95 feet (29 meters) with a cross-cut driven northward 35 feet (11 meters) at a depth of 60 feet (18 meters)
1900: The English Company had difficulty raising the money required to build a 100 stamp mill. The property reverted back to the crown.
1926: Mr. H.K.Bridger staked six claims covering the Alice"A" and optioned them to G.B.Butterworth. Butterworth formed an association known as "The Mining Group" to provide financing. Development work includes trenching, pitting and cleaning out old open cuts and shafts for test purposes.
1980: Property was staked by Redding.
1982: Property was staked by B.Portelance of Thunder Bay,Ontario.
1983: The Property owner is presently unknown. Contact person is B.Portelance of Thunder Bay, Ontario.
Geology and structure of the mine i
The Alice"A" prospect is situated between the east-west trending Quetico Fault and the northeast-northwest trending Seine River Fault. The area is underlain by steeply dipping east-west striking , felsic to mafic volcanics. The raetavolcanics are composed of sericite-chlorite-carbonate schists which may have originally represented a sheared and silicifed rhyolite flow or a felsic fragmental rock such as a tuff or lapilli-tuff. Mafic metavolcanics, present as chlorite schists are encountered on the north portion of the property. Shearing is prominant throughout the Alice"A" property, the shearing strikes east-west with dips of 80 degrees north to vertical.The shear zone was observed to be approximatly 90 meters in width, however,
old reports indicate a width of 800 feet (244 meters). The Alice"AH property is located approximately 0.5 km. south of the east-trending Quetico Fault.
Mineralogy of the Mine:
Quartz-carbonate veins and stockwork appear associated within east-trending lenticular shear zones. The host rocks are felsic to mafic pyroclastic rocks. The quartz-carbonate veining is very erratic varying in width from l cm to over 20 cm and shearing but more or less parallel to the shearing. Visible mineralization consists of pyrite, chalcopyrite, galena, sphalerite and gold with accessory minerals including sericite, chlorite and carbonate.
-4-
Economic features of the Mines
Tonnage and grade estimates; 1898 initial reports indicate that the for mation was gold bearing throughout, over a width of 800 feet. Speculation on a low grade, large tonnage operation is recorded. A aill test in 1898 of 10 tons of unsorted material taken from both shafts and various test pits gave an average value of $10.80 per ton.Further milling of samples from various workings gave results from $2.00 to $64.00 per ton and an average of $12.00 gold and a small silver value.
Previous Property work
1975 Hanna Mining completed a magnetometer,GEM and MaxMin II surveys plus a geological mapping and diamond drilling program over the western portion of the property.
GRID-LINECUTTING
An exploration grid totalling 117km was cut over the entire property (40-K)OWest-43*OOEast). A baseline was cut in an east-west direction with wing lines perpendicular to the baseline at 100 meter Intervals.Chained stations along the baseline and wingllnes were established with a 25 meter spacing.
,
r.: .-5-
MAGNETIC SURVEY(2)
Instrumentation
The survey was performed using a Scintrez MP-2 portable proton-precession magnetometer.A Scintrex MBS-2 magnetic base station was used to record and correct for diurnal variations.
The MP-2 has an accuracy of -f/-l gamma in a field of 50,000 gammas. However,actual survey accuracy is proportional to the degree of care used in applying diurnal corrections.
Theory of Operation
Magnetic variations are caused by variations in magnetization of the rock from station to station.This magnetization exists because of the presence of minerals with high magnetic susceptability.The most common minerals to affect the earths magnetic field are magnetite,pyrrhotite,and ilmenite. Magnetometers are used to measure this variation.
The MP-2 is a proton precession magnetometer.This magnetometer utilizes the precession of spinning protons in a volume of kerosene to measure the total magnetic field intensity.
When the hydrocarbon is subjected to an electric current the spinning protons are temporarily polarized.When the current is removed the spin of the protons causes them to precess about the direction of the ambient magnetic field.The signal generated by the processing protons is directly proportional to the intensity of the total magnetic field.The magnetic intensity measured is the magnitude of the earths magnetic field vectorindependant of its direction.A change In the total field intensity is referred to as an anomoly.
Survey Procedure
Data was collected at 25m intervals using a Scintrex MP-2 proton mageto- meter.Field data was then referred to the log of a base station recorder ( Scintrex MBS-2 ) which operated continuously throughout the survey for correction.The corrected data is plotted at a scale of 1x2500 and contoured.
Discussion of Results
The Proton Mangnetometer Survey conducted over the property was very useful in outlining its many magnetic trends. In general there are three major magnetic trends present on the property; 1) The Main Zone 2) The South Zone and 3) The Southwest Zone.
The Main zone is a broad magnetic expression located between 3+00 south and extends the entire length of the property. It is approximately 500 to 600 meters wide and probably represents a volcanic flow and/or tuff bearing disseminated magnetite or pyrrhotite.
An interesting morphological feature of this trend Is the "lobes" which appear along the northern boundary of the unit. These lobes appear to be related to the unit but have somehow been pinched away from the trend. It is felt that these feature's are probably structurally related and possibly
-6-
due to a cross folding of the unit. The data along the southern boundary of the unit is incomplete and it is impossible to say whether these features were repeated there. Since these lobes appear to be strucurally related, the anomalies found within them ("J" "K" and "E" ) could present interesting exploration targets.
The several anomalous trends found within this main zone are described as follows:
Trend "A" is located on lines 17E to 43E between 2+00 and 3+00 South. It has a strike length of greater than 2700 meters with the highest values being on lines 21E and 25E (2200 gammas). It is overlapped by trend "B" on lines 17E to 22E (actually this overlap may be due to an entirely seperate trend but has been included in "A" for this discussion.) Unfortunately the data on trend "A" is incomplete and the magnetics over the south half of the trend was not available due to the position of the grid . The width of the trend seems to be fairly broad so it is thought that this may be to a magnetic or sulphide bearing horizon within a main volcanic unit.
Trend "B" is located directly above "A" and is found between lines 22E and 4W. It has strike length of 2600 meters and is positioned along the baseline at 0+00. The highest values (2400 to 3000 gammas) are found on lines 13E to 16E and lines 19E TO 20E. This trend is believed to be mineral ogical ly similar to trend "A".
Trend "C" la a long discontinous anomaly between lines 9E to 17W. It has a strike length of approximately 2600 meters and is found between 1-200 north. The best responces are on lines HW to 17W (3000 to 5000 gammas). The responce is broad and it is believed the high values within this trend are due to a narrow magnetic and l or sulphide enriched horizon.
Trend "D" is a short anomaly which is located on lines 2E to 3W at approxi mately 1+00 South. It has a strike length of about 500 meters with the highest value (2000 to 2300 gammas) being on lines IN and 2W. This relatively short trend could be interesting depending on which exploration model one is working with.
Trend "E" is one of the anomalies that occurs in a "lobe" which was discussed in the introductory comments above. Like"D", this trend has a relatively short strike length (700 meters) and Is made all the more attrac tive by its spatial relationship to the rest of the main zone. It occurs between lines 18E to 25E and between 3+50 and 4+50 North with the highest values being on lines 19, 23 and 24E. The low values would seem to indicate that the anomaly was due to a sulphide rather than an oxide assemblage.
Trend "F" is an incomplete responce as it strikes off the west edge of the grid. Itis located beween 2-2+50 North and the highest values are between 1500 and 1800 gammas. This anomaly is probably due to disseminated sulphides or magnetite.
Trend "G" is open at both ends and is located along the lower contact of the main zone between lines 29W and 40N (1+00 to 2+00 south). It Is similar to the majority of the trends on the grid in that it has a number of discon tinous high values (up to 2700 gammas) along its strike length and is fairly broad. These magnetic highs may represent different parallel horizons within the trend. The lower values and the dipole on line24W would seem to indicate that the anomaly is due to a sulphide assemblage (ie.pyrrhotlte/pyrite).
Trends "J" and "K" have relatively short strike lengths and like "E" are found in one of the structural "lobes" between lines 15N to 21N (2+50 to 3+50 north). They have lower values (1500 to 1900 gammas) and may represent
-7-
interesting targets for the reasons previously discussed.Trend "L" is a one line dipole responce on 23W, 1+00 south.It is open
to the east and probably to a suphide assemblage.The southwest zone is another broad unit loosely separated from the main
zone by a narrow band of 900 gamma values. It has two anomalies of significance within it , "H" and MFF".
Trend "H" is a wide responce and open to the west. It is located on lines 37W to 4OH between 5-1-00 and 7+00 south. This trend is different from the usual type of responce found on the grid in that its values are marginally higher and they occur over a greater width. This greater width may be due to structural thickening during deformation of a mineralized horizon. I would be inclined to say that magnetite may be the primary cause for this trend.
Trend"FF" is a two line responce which is very similar in morphology to "H". It is located on lines 28W and 29W at 7-1-00 south and is by far the strongest responce on the grid. Its high gamma values are probably due to magnetite.
The south zone is found on lines 4W to 6E at about 9-1-00 south and is open at both ends. It is not as discontinous as most of the other trends and is fairly narrow and well defined between lines O to 4W. The values are slightly higher for this anomaly (2000 to 3400 gammas) however it is difficult to say whether a magnetite or sulphide assemblage is the cause of this trend.
There were only two anomalies due to culture on the grid and both were caused by the CPR railway tracks which cut the southwest and southeast corners of the property. The usual precautions should be taken when looking at any data around the many bush roads which criss-cross the claim block.
All in all the magnetic survey was extremely useful in dellniating a number of interesting geological feature's on the grid.
-8-
ELECTROMAGNETIC SURVEY{2)
Instrumentation
A VLF-EM survey was performed using a Geonics EM-16 unit.A Crone Radem VLF-EM unit was used between L-40+OOW and L-34+OOW.
Theory of Operation CEM163
VLF-transmitting stations operating for military communication have vert ical antenna.The vertical antenna creates a concentric horizontal magnetic field .When these magnetic fields encounter conductive bodies in the ground, a secondary field is created.The VLF receiver measures the vertical components (inphase and quadrature) of these secondary fields.
The EM-16 is a sensitive receiver covering the frequency bands of the VLF-transmitting station with means of measuring the vertical field components.
The receiver has two inputs,with two receiving coils built into the instrument.One coil has normally vertical axis,the other is horizontal.
The signal from one of the coils (vertical) is first minimized by tilting the instrument.The tilt angle is calibrated in percent.The remaining signal in this coil is finally balanced out by a measured percentage of a signal from another coil,after being shifted by 90 degrees.
Thus if the secondary signals are small compared to the primary horizon tal field,the mechanical tilt angle is an accurate meaure of the vertical real-component,and the compensation 90 degree signal from the horizontal coil is a measure of the quadrature vertical signal.
Survey Procedure CEM163
Readings were taken at 25m intervals over the entire grid.Both the dip angle and the quadrature were noted at each station.The transmitting station used was Cutler,Maine.
To take a reading the refrence coil ("T") in the lower end of the handle is oriented along the magnetic lines 90 degrees to the station direction.This is acheived by swinging the Instrument back and forth until a minimium sound intensity is heard.The quadrature dial is then adjusted until the sound is further minimized.The dip is then read from the inclinometer and the quadrature from the dial.The same direction is always faced when readings are taken.
Discussion of Results
Unlike the Proton Magnetometer Survey the VLF Survey was not very success ful in defining any conductive zones as good exploration targets.
The majority of the grid is very flat and swampy and as a result is prone to producing anomalies which are essentially caused by conductive clays found in the old river channels, shears, ect.
The anomalies which were located by the VLF tended to be broad and reflee- ing a river channel type of responce rather than a bonafide bedrock conductor.
-9-
This of course does not mean that every conductor on the property should be written off as a topographic responce, however the data has to be looked at very carefully in order to sort these problems out.
Actually very few VLF responces corresponded to the major magnetic trends. The conducters, in many cases, cut across the trends rather than to follow them with only one or two crossovers seeming to correlate with the magnetic highs. This situation creates a problem in trying to grade the conductors since one is left with no clear answers as to what might be the cause of the anomalies. The quaderature will help to some extent however a detailed geological survey in the vicinity of some of these conductors hopefully will sort some of these problems out. Unfortunately sufficient outcrop exposure will be a problem in this area so one may be forced to do a more expensive geophysical survey such as IP in order to resolve these difficulties
The data between lines 33W and 40W was collected using a Radea VLF and as a result there is no quaderature data collected over these lines. It should be noted that the frazer filtered values produced over these lines will be lower because of the difference in measurements between the Radem and-.the Geonics system, ( The Radem measures dip angle in degrees while the Geonics EM-16 measures the dip in precent).
A complete list of all the VLF conductors with there relative comments can be found in the next section.
TABLE OF VLF RESULTS
-ID-
OjJN
A
B
C
D
E
F
G
H
I
LOCATION STRIKE FILTER LENGTH RESPONSE METERS
30W TO 15W S1500+ ! FAIR TO 7+00 - 7+50! ! POOR
NORTH ! !
31W TO 23W ! 800 5 FAIR TO 4+50 - 5+50! ! POOR
NORTH ! !
30W TO 10W 12000 5 GOOD TO 1+50 - 3+00! ! POOR
NORTH ! !: t i ii it it i i ii tt it i i ii i
33W TO 30W I300+ ! GOOD TO 0+75 - 1+25! ! POOR
NORTH ! ! t i
30W TO 33W 1300+ 1 POOR TO0+25 - 0+75! ! FAIR
i ii i
*33W ! ONE ! FAIR 2+50 SOUTH ! LINE !
33W TO 23W I1000+ J GOOD TO 4+00 - 4+50! I POOR
SOUTH ! ! i t i ! 1 ! i t
33W TO 29W I400+ ! FAIR TO 6+00 - 7+00! ! GOOD
SOUTH ! !
33W TO 31 W J200+ ! FAIR TO 8+00 SOUTH ! ! GOOD
PROFILE RESPONSE
POOR
POOR
POOR
.
-
POOR
FAIR TO GOOD
POOR
FAIR TO GOOD
GOOD
FAIR
MAG
NO
YES
NO
YES?
NO
YES
NO
NO
REMARKS
THIS CONDUCTOR IS PROBABLY DUE TO THE TOPOGRAPHIC ANOMALY CAUSED BY THE RIVER
VERY MINOR MAG LOW WITH THIS CONDUCTOR (APPRO X 200 GAMMAS)
A LONG SINIOUS CON DUCTOR WHICH HAS A NUMBER OF SPOT HIGHS ALONG ITS STRIKE. LINES 17W, 13W AND 12W ALL HAVE GOOD FILTER RESPONSES.
THESE HAVE PROBABLY BEEN ENHANCED BY THE RIVER HOWEVER THERE
IS A MAG HIGH OF 1500 GAMMAS WITH THE RESPONSE ON LINE 17W
BEST FILTER RESPONSE ON LINE 32W. NO MAG
TO SPEAK OF. OPEN TO WEST
FLANKS THE NORTH OF A MAG TREND OF 2700 GAMMAS. NO REAL ONE TO ONE CORRELATION
HOWEVER
ONE LINE RESPONSE AND OPEN TO THE
WEST
OPEN AT BOTH ENDS POSSIBLE MAG COR
RELATION ALONG THE NORTHERN BOUNDARY OF THE SOUTHWEST TREND < ROUGHLY FOLLOWS THE
BREAK)
OPEN AT BOTH ENDS
OPEN TO THE WEST SIMILAR TO "H"
F,
TABLE OF VLF RESULTS-11-
CON LOCATION STRIKE FILTER PROFILE LENGTH RESPONSE RESPONSE METERS
MAG REMARKS
ssssss
J
K
L
M
N
NN
0
P
Q
Q DO
6W TO 12W ! 600 S FAIR TO 0+00 - 0+50! ! POOR
NORTH i !
5W TO 6E 11 1+00+1 POOR TO 1+25 - 0+25! 5 FAIR
SOUTH j !: 5 : :
*5W TO 6E 511+00+5 POOR TO 3+50 - 5+005 5 GOOD
SOUTH 5 !
0+00 TO 4W 54+00+ 5 POOR TO 5+50 - 6+50! 5 FAIR
SOUTH 5 ! ! ! 1 I
3E TO 5E ! 200 ! POOR TO 4+00 - 4+25! 5 FAIR
SOUTH ! 5
'5W ! ONE 5 POOR 2+50 SOUTH ! LINE !
0+00 TO 1W ! 100 ! POOR 8+25 - 8+00! !
SOUTH 5 ! i !
5E TO 6E l 1+00+ ! POOR 7+50 SOUTH 5 !
! i
2E TO 6E 54+00+ ! FAIR TO 10+00 SOUTH! l GOOD
i !I !
*"6E I1+00+ ! POOR 9+25 SOUTH ! !
; i : i
3W TO 4W I1+00+ ! POOR 9+25 SOUTH ! !
5 I
POOR
POOR
POOR
POOR TO FAIR
POOR
POOR
POOR
POOR
FAIR TO GOOD
POOR
POOR
NO
YES?
NO
?
7
NO
NO
NO
?
YES
YES
TOPOGRAPHY?
OPEN AT BOTH ENDS VERY WEAK CONDUCTORS ALONG THE NORTHERN
FLANK OF LINES 0 TO 2W
POSSIBLE ENHANCEMENT BY TOPOGRAPHY
OPEN AT BOTH ENDS
OPEN TO THE WEST POSSIBLE CORRELATION ON THE NORTH FLANK OF A SMALL MAG HIGH ON LINES 1 AND 2W
POSSIBLE FLANKING MAG TO THE NORTH. MINOR RESPONSE
SWAMP?
INTERESTING IN THAT IT LIES JUST TO THE NORTH OF A MAJOR MAGNETIC FEATURE
VERY MUCH THE SAME AS CONDUCTOR 'O* OPEN TO THE EAST
LIES TO THE SOUTH OF A MAJOR MAGNETIC
TREND. HAS FAIRLY GOOD CONDUCTIVITY.
OPEN TO THE EAST CORRELATES WITH A
MAJOR MAGNETIC TREND VERY WEAK
VERY MUCH THE SAME AS "QQ" CORRELATING
WITH THE SAME
TABLE OF VLF RESULTS
-12-
CON LOCATION STRIKE FILTER PROFILELENGTH RESPONSE RESPONSE METERS
MAG REMARKS
i
t
J
i
\
t
Z
A
8
! ! 1 ! !
2W TO IE J3+00+ i POOR TO 11+50 SOUTH! ! FAIR
0 TO 6W ! 600 ! POOR TO 11+50 TO ! ! GOOD
'11+75! ! NORTH ! !
3W TO 4E ! 700 S FAIR TO 9+50-10+00 ! ! GOOD
NORTH ! !
4E TO 6E 5200+ ! GOOD 11+50-12N S !
2W TO 9W ! 700 ! FAIR TO 7+50 - B+00! ! GOOD
NORTH ! !
3E TO 5W ! 800 ! FAIR TO 6+50 - 7+00! t GOOD
NORTH ! !
IE TO SE ! 700 ! POOR TO 4+50 - 7+00! ! GOOD
NORTH 1 !1 11 1
i !
4E TO 7E ! 300 S POOR TO 3+25 - 3+50! ! FAIR
NORTH ! i
4E TO 9E ! 500 ! POOR TO 2+25 - 2+50! ! FAIR
NORTH ! !
6E TO 7E i 100 ! FAIR 3+00 NORTH ! !
! i ! l
9E TO 12E ! 300 ! POOR 5+50 - 6+00! !
NORTH ! !
15E TO 1BE ! 300 ! FAIR TO !
POOR
POOR
POOR
POOR
POOR
POOR
POOR
.
POOR
POOR
POOR
POOR
POOR
NO
NO
NO
NO
NO
NO
NO
NO
NO
.
?
NO
NO i
MAGNETIC TREND. VERY WEAK
SWAMP?
SWAMP?
SWAMP?
CORRELATERS TO ROAD
TOPOGRAPHIC
COULD BE INTERESTING BECAUSE OF LOCATION (IE. NOT IN A SWAMP)
THE GOOD RESPONSE OF THIS TREND COR
RELATES TO THE ROAD. VERY WEAK PROBABLY CAUSED BY SWAMP.
PROBABLY CAUSED BY THE RIVER
SWAMP?'
CORREALTES WITH A MAG TREND AS WELL AS A LOGGING ROAD POSSIBLY CULTURE.
PROBABLY CAUSED BY THE RIVER
SAME AS 'AA'
u
w
-13-
TABLE OF VLF RESULTS
CON LOCATION STRIKE FILTER PROFILELENGTH RESPONSE RESPONSE METERS
MAG REMARKS
CC
DD
EE
FF
GG
HH
II
JJ
KK
17-1-50 - 8+00! NORTH
12E TO 15E10+50-10+00
NORTH
22E TO 30E7+00 - 8+00
NORTH
21E TO 24E4+25 - 5+25
SOUTH
23E TO 43E1+75 -3+00
NORTH
31E TO 43E3+75 - 5+50
NORTH
39E TO 40E6+00 - 6+50
NORTH
29E TO 38E6+50 - 7+00
NORTH
18E TO 20E 10+75 NORTH !
!l!
18E TO 20E !1+00 SOUTH !
!
S ! POORt ;! 300 S POOR1 !: ii :800+ ! GOOD TO
! POOR!
300 ! POOR TO! FAIR!1
2000+ ! FAIR TO1 GOODi i5t
!ii
1200+ 1FAIR TOl GOODl 11 l
100 ! FAIR!i
900+ i POOR!!
200 ! FAIR!!!!
200 ! FAIR TO! POORt
FAIR
POOR
POOR
POOR TOFAIR
POOR TOFAIR
POOR
POOR
POOR
FAIR TOPOOR
NO
NO
?
NO
NO
NO
NO
?
?
INTERESTING IN THATTHE CONDUCTIVITYIS SLIGHTLY BETTER
THAN 'AA' AND 'BB*.
OPEN TO THE EASTPROBABLY CAUSED BY
THE RIVER.
OCCURS ON THENORTH FLANK OF ONEOF THE MORE INT
ERESTING MAG TRENDS.
OPEN TO THE EASTA VERY LONG AND
FAIRLY STRONG CON DUCTOR. SPLITS AT 32EAST, POSSIBLE TOPO
ANOMALY AT THISPOINT.
OPEN TO THE EASTVERY SIMILAR TO 'FF'BEST CONDUCTIVITYAROUND LINES 32-33
SWAMP?
SWAMP?
SWAMPY GROUND, HOW EVER IT IS FOUNDON THE NORTHERN
FLANK OF A MAGNETICTREND.
MUCH THE SAME AS 'JJFOUND BETWEEN TWO. MA
EXPRESSIONS.
-14-
REGIONAL GEOLOGY
The Alice"A" property occurs in the Atikokan-Fort Frances greenstone belt of Northwestern Ontario.This property is located in the Wabigoon Sub- province and is struct
REGIONAL GEOLOGY
The Alice"A" property occurs in the Atikokan-Fort Frances greenstone belt of Northwestern Ontario.This property is located in the Wabigoon Sub- province and is structurally located south of the Quetico fault.This area consists mainly of felsic and intermediate volcanics.The "Seine River Series" clastic metasediments are situated to the south of this greenstone belt with the Irene-Eltrut Lake Batholith!c complex.
PROPERTY GEOLOGY
The major problem associated with the compilation of a geological map for this property is related to the low percentage of outcrop.A general overview is possible based on geological,magnetic and EM interpretations.
Rock types outlined in the following list represent lithologlcal units mapped on the Alice"A" property.These rock types will be discussed in the same order as ascribed below. References are made to the geology maps that are provided with this report.
VOLCANICS:————————— 1) MAFIC VOLCANIC
2) INTERMEDIATE VOLCANIC3) FELSIC VOLCANIC
METASEDIMENTS—————————— 4) BANDED IRON FORMATION
PLUTONICS————————— 5) MAFIC INTRUSIVE
6) FELS1C-INTERMEDIATE INTRUSIVE
1) Mafic volcanics comprise a relatively small percentage of the rocks exposed on the property. The most easterly segment of the grid (le.map l of 4) near the baseline reveils a medium grained massive mafic volcanic with minor pyrite mineralization.This may however, be an intrusive (le.gabbro).Other occurences of mafic volcanics tend to be interfingered with intermediate volcanics and it is thought that these may in fact be part of the same litho- logical sequence. The differences may be explained by an alteration or colour phase within the lithology.
2) There are three areas of intermediate volcanic outcrop on the property. The first area(on sheet 3 of 4) is near the southern boundary of the property around line 5+OOeast. This strongly foliated intermediate volcanic is medium to fine grained. Mineralization is isolated to fracture planes with minor pyrite and carbonate.The second area of outcrop extends over sheets 3 and 4.This intermediate-
volcanic is interfingered with felsic volcanics and a banded iron formation near line 14+00 west, just north of the baseline.Characteristle features include, highly stretched quartz eyes and banded volcanics in segments.
-15-
Minor pyrite mineralization is also present.The third area where intermediate volcanics occur are north of the baseline
near line 28+00 west.This intermediate-mafic volcanic is fine to medium grained in texture with a strong foliation. Both pyrite and carbonate mineral ization are observed on fracture planes.
3) Felsic volcanics are the most abundant rock type exposed on the property. They are mainly exposed south of the baseline and in many instances are Inter bedded with intermediate volcanics. The majority of the felsic volcanics are tuffaceuos in nature and in some outcrops they are siliceous and crystalline. Texture is variable throughout this unit from medium grained to crystalline. The degree of foliation varies from both extremes.Minor pyrite mineralization occurs throughtout lithologies with quartz stringers and carbonate fracture filling.Sericite alteration was observed in highly foiliated to crystalline rocks exposed near L-24+OOW and south of the baseline.All units have an east- west strike and a steep to vertical dip.
An area of abundant outcrop south of the baseline between L-23+OOH and L-26+ OOW, exposes felsic tuff to felsic crystal tuff on strike with the Alice"A" prospect.These strongly foliated to schistose rock are very similar in appear ance to those at the Alice"A".
4) Banded Iron Formations outcrop in two areas on the property.On L-3+OOE near 5+50N there is a BIF within an intermediate to felsic volcanic.This iron formation contains bands of chlorite with stringers of quartz and pyrite.Adjac ent volcanics are contorted and folded with fine grained stringers of pyrite and quartz.The second banded iron formation is located near L-14+OOH and 1+OON this lithology displays the same pysical attributes as the previously describ ed.
5) The most easterly part of the grid,north of the baseline, exposes an area of mafic intrusive rocks.This rock unit is isolated in size and is associated with felsic dykes.These mafics are massive and fine to medium grained.
6) A granite body was observed in the middle of the grid north of the Little Turtle River.This intrusive body is thought to be related to the Irene-Eltrut Lake batholithlc complex to the north.The southern contact is identified with metamorphosed felsic volcanics on L-l+OOW at 6+75N.A18O identifed within the contact zone (le. to the west) are mafic volcanics.Where observed, the economic potential of the contact zone does not seem significant.
SUMMARY PROPERTY GEOLOGY
The geological base maps produced during the summer of 1984 lack a great deal of outcrop and as such de not represent a good geological picture.In terms of the potential for economic mineralization, emphasis should be placed on the more felsic to intermediate volcanics that exibit greater mineraliza tion. Although no significant mineralization was observed and assay results were not encouraging the lack of outcrop may aid in explaination.
-16-
SAMPLE DIARYAU AU
TAG # oz ppb
111371113811321113221132311324113251140111402114031140411405114061140711408114091141011411114121141311414114151141611417114181141911420'11421114221142311424114251142611427114281142911430114311143211433114341143511436[114371143811439
11440
12529ndndnd5
ndndndndndndndnd51ndnd9nd2161114nd5ndnd12ndndndndndndnd12ndndndndndnd4628
101
LOCATION
25+OOe21+OOe39+25639+OOe.39+OOe2+9063+60612+lSw12+2512+60W12+45W12+lSw12+OSw5+55W4+lOw4+0 Ow3+2 Ow4+02W4+OSw3+95W3+OOw3+OOw3+25W2+3862+3863+lOe3+lOeO+BSe1+2562+SOe2+5562+lSe3+2563+25620+lOe12+85W13+OOw13+OOw13+75W23+OOw24+90W16+lSw28+78W4+1 2w42+OSe42+306
42+OSe
6+2006+OOn3+SSn6-f25n3*25nl+75n2+eSn0+SOn0+SSn0*75n1+SSnl+25n1+OSn10+75811+40312+SOs12+OSs5+1585+1584+2585+2085+2585+2585+1 On5+lOn5+SOn5*90n8+2508+gOn5+SOn5*52n5+SOn5*40n5*90ni+gon1+SOnmOn0+75n0+lSs0+55&1+7580+SOs5+8207+SOn3+1283+lSs
3+208
DESCRIPTION
mafic-inter*. intrusive, trace pyfelsic intrusive, trace pyritemafic volc.bnded,qtz stringersinter-mafic vole, qtz eyes, H. A.mafic vole., well bnded, foliatedchlorite schist pyriteinterm.volc py, platy foliationSen qtz vein in felsic xtal tufffei xtal tuff network qtz veiningtrench - int vol minor sulfidepy,fe stain int. vol. qtz eyes.int. vol. blue qtz eyes minor py.qtz vein 7.5cm in felsic tuffqtz vein in int. vole (poss. float)qtz vein 2-3cm carb,fe-stainqtz vein l-3cm,int vole qtz eyesq.v.2cm with tourmaline int/felq.v 15cm, ser. f el. vole, pyas 11411q.v. se.r.fel.tuf py,chl,fe-stainq.v. lcm f el. vole. py,fe-stainsil . f . g. f el . tuff , carb, f e-stainq.v. in f el. tuff f e-staincont. f el-mafic >80%Si,py, bnded3\py cherty sed,ep,ser,hem alt.b. i. f. < *7Q\ mag,po.q.v. network in gabbro? carb.maf .vole, in cont. with grdior.maf .vole, away from cont.min.py4cm qtz vein,chl,felds,ep,8ll.fel.volc.ep,l-2% dlss.pym. g. maf le vole. ,ep,py, contortedB. I. F. south sample 705k*ag,2*pyB. I. F. north sample see 11426mafic vol c. carb (s id?) ,pycontact int-f el . strong fol.carb.M. A. maf -int. vol c. py, carb.B. I. F. in sheared in t. vole. py, cblq.v. stock. in f el. tuff ,py,carbfei. tuff ,blk, ser, q.v. fe stainq.v. contact f el -maf vole.q.v 10cm in fei vole. ,chl,fe.q.v. 3cm in mafic vole. 5%pymaf .pendant in diorite, contactf el. xtal tuf. cherty, ser, carb, pycherty contc.zone fel-int.volcbnded mln diss-f string. pyriteint. vole, carb, min. pyrite
114411144211443114441144511446114471144811449114501145111452114531145411455114561145711456118011180211803118041180811809
ndnd232ndnd245ndndndndndnd239nd151169ndndndndndnd59
-17-
41+OSe 3+SOs int.vole,M.A.carb in fractures28+986 4+SOn alter.fel.intr.O*py,10*biot-chl30+35W 5-f90n gabbro,*.g.cumulate texture,5\py32+176 6-K)2n gabbro/felsic dike contact,O\py33+OOw 2+eSn mafic vole. ,f .g. weak fol.,py36+OOe 4-f22n felsic dike in maf .vole,f .g. ,py38+OOe 2*65n int.vole.blue q.eyes,q.strings.40+OOe 3+SBn mafic-intern.vole.,banded5-i-85e 8-t-SOs intern.vole. ,^py,carb.fracturesH-05e 12+SOs fei.vole.,4cn q.v.,minor py.1+92W 10-f25s qtz.vein,2cm,in felsic vole.
41-fOOe 3+OOn intern.volc.<4%py,carb.fract.43+OOe 2-t-25n intern, vole. 3*py, carb, fractures42-1-856 3-i-75n int. vole. carb, f rae, 12\ py-cpy0+85W 12+OOn granodiorite,blot.rich,gneissic
33-fOOw 4-i-38n maf .vole, alter. <10% py,q.v.33+OOw 4-*-73n BIF,<10% nag in q.v.34-fOSw 3+eOn q.v.pod in maf .gneiss2+OOw 4+338 intern.vole chlorite alter.2+lSw 4+35S??? float-qtz vein23+036 4+48n mafic vole.,carb-silic-pyrite22+826 3*90n felsic tuff,bnded,silicified,py21+SOe 6+eSn intermediate intrusive28+OOe 4+45H gabbroic intrusive
BASAL TILL SAMPLING
A basal till sampling program was conducted during the fall of 1984. The basal till sample is a sample of till taken from the lower till and bedrock Interface. This sample is obtained with the aid of an overburden drill. Geochemical anaysls is determine through two processes. First process deals with an atomic adsorption analysis of the till selved to a -250 mesh size. The second process and other half of the original sample is put through a heavy metal separation and then analyzed for AU,CU,ZN,AG. Results from the program are listed in the table below.
SAMPLE* LOCATION DEPTH TILL HEAVY PULP HEAVY(wt./gr)
3201320232033204320532063207320632103211321432153216321732183219322032213222322332243225
31+OOW/1+25S31+OOW/l+OOS31+OOW/0+75S31+OOW/0+50S29+OOW/6+25S29+OOW/6+50S29+OOW/6+75S29+OOW/7+OOS30+OOW/5+OON30+OOW/5+25N30+OOW/6+OON30+OOW/6+25N1+OOW/1+25S1+OOW/0+05S1+OOH/0+75S4+OOW/1+75S4+OOW/1+50S4+OOW/1+25S3+OOW/4+OOS3+OOW/3+75S3+OOW/3+50S3+OON/ 3-1-253
17.114.112.15.114.114.09.1
18.411.15.1.9
1.89.1
15.118.15.1
12.014.02.08.18.09.0
342
1631
198
1375211
151841431
1101
3173
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3.831.722.991.123.884.334.227.97
.905.882.65
6.508.83.96
3.906.40
2.532.031.80
F
SUMMARY OF EXPLORATION
This report details the results of a major exploration program undertaken by Lynx Canada Explorations Ltd. Surveys include complete coverage of all claims with linecutting,VLF-EM,magnetometer,and geological surveys.In addition to this a basal till sampling program was undertaken to test various targets. A diamond drill program is pending at this time based on more basal till sampling and the results of such sampling.
CONCLUSIONS
1. Due to a lack of outcrop on the property, a full understanding of the geological environment based on the mapping program was not possible.However, the geophysical (le.magnetometer 4- VLF) surveys suggest an east-west trend that allows one to infer structural and geological horizons.Thus, If one combines geology and geophysics a more general senario can be deduced. This senario Is still very general for gold exploration.
2. The basal till sampling technique is a good method for sampling in areas with excessive overburden.An overburden situation was the case for most of the geophysical anomalies on this property. The proximity of the sample location with respect to the bedrock and till interface, results in a sample analysis that is a good representation of bedrock. Some anomalous values were obtained through the basal till method.
RECOMMENDATIONS
1. Although a good deal of work has been done on the Alice "A" property there is still not a good deal information about its geological environment. Therefore, it is thought that there is still a need to collect data and to prove/disprove anomalies outlined in this preliminary phase. Possible methods to meet this end could Include, more detailed geophysics and more advanced techniqes for better definition of anomalous zone.
2. Further basal till sampling on anomalies previuosly tested with higher than background values plus, areas untested may lead to increased knowledge of areas.
3. Ultimately diamond drilling will prove/disprove anomalies in terms of there gold potential. A drilling program should only be undertaken once other less exspensive methods have been exhausted and have outlined anomalies worthy of such a program.
F
REFERENCES
I.Ontario Geological Survey,Assessment Files, Toronto,2.Phantom Explorations,Thunderbay.3.Lynx-Canada Explorations, in file reports.
SUBMITTED BY:
PETER MORDAUNT JANUARY 1985
52Ct6SEMOS 63.4866 BENNETT
163. y 808l of Z-
OM 83-3-C05Y
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THIS SUBMITTAL CONSISTED OF VARIOUS REPORTS, SOME OF WHICH HAVE BEEN CULLED FROM THIS FILE. THE CULLED MATERIAL HAD BEEN PREVIOUSLY SUBMITTED UNDER THE FOLLOWING RECORD SERIES (THE DOCUMENTS CAN BE VIEWED IN THESE SERIES):
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Scale : l: 50,000 N.T.S. 52-C- 16
MAGNETOMETER SURVEYINSTRUMENT: SCINTREX MP-2 PROTON MAG. DATUM : 59,000CONTOUR INTERVAL: MAGNETIC LOW : CZ^
BASE STATION RECORDER INFORMATION INSTRUMENT: SCINTREX BSR -2RECORDER RANGE : 100 CK RECORDING INTERVAL : 10 SECONDS CHART SPEED: 22 MM/SEC.
VLF SURVEYINSTRUMENT : GEONICS EM - 16 TRANSMITTING STATION: CUTLER, MAINE DIP ANGLE : - ——— -——— - ——— - QUADRATURE : PROFILE SCALE : CONDUCTOR AXIS ; POSITIVE READINGS EAST OF LINE CONTOUR INTERVAL :
TOPOGRAPHY
CLAIM POST :
CLAIM LINE :
SWAMP: ^
SWAMP BOUNDARY :
RIVER :
ROAD :
RAILROAD:
LYNX CANADA EXP
MAP 3/4
lORATlONS LIMITED
ALICE "A" PROJECTLITTLE TURTLE RIVER AREA
DISTRICT OF RAINY RIVER
Date : April ,I984 Scale : l : 2500 NT.S. 52 -C- 16
PHANTOM EXPLORATION SERVICES LTD.
