42A10SW0272 2 .5554 MACKLEM 010
REPORT ON 1982 REVERSE CIRCULATION
ROTARY OVERBURDEN DRILLING
PROGRAMME - MACKLEM TOWNSHIP,
GOLDEIDT EXPLORATIONS INC.
R. Sibthorpe, B.Sc. May 17, 1983
RECEIVED',\.tf i B '̂
NDWNO LANDS SECTION
WrROpUCTIpN
From August 21st to 27th, 1982 a 10-hole dual tube reverse circulation rotary overburden drilling programme was carried out on the Macklem-Bond Township property of Goldeidt Explorations Inc. by Heath de Sherwood Drilling Limited under the supervision of Messrs. R.E. Routledge and R. Sedore of Derry, Michener, Booth (5c Wahl (DMBW). Six of the ten holes drilled were located on patented claims held
under option by Goldeidt Explorations Inc. The four holes drilling on unpatented claims held by the company are the basis of this report. A proportionate amount of the total program costs have been claimed for assessment purposes.
This report has been compiled by Robert Sibthorpe from several reports sub mitted by consulting firms to Goldeidt Explorations Inc. The author graduated from the University of Toronto in 1972 with a Bachelor of Science in Geology and has been engaged in mining and exploration work since that date. He directed and supervised the work program.
LOCATION AND ACCESS - Figure l
(NTS 42A10; longitude 80 47'32W - 80 54'30W; latitude 48 28'25N - 48 37'30N)
The property is located 35 km east of Timmins, Ontario, in central Macklem and west-central Bond Townships, Porcupine Mining Division, District of Cochrane. Regularly scheduled airline service is available at Timmins. The claim group is accessible by all-weather highway #101 and the Gibson Lake Road. The Gibson Lake Road departs from highway ft 1 01 at 38 km east of Timmins and traverses the east- half of the property, about 3 km south of the highway. The access road to the former Miller Paving Gravel Pit leads 1.5 km to the drill area centered at the intersections of claims P23054, P23055, P486668 and P486672. A number of old lumber haulage and skidder roads as well as newly cut north-south picket lines cut at 400 ft. intervals provide good access in the area drilled.
DESCRIPTION OF THE OVERBURDEN DRILLING PROGRAMME
Holes were spotted on the 22nd of August at 200 ft. to 400 ft. intervals north of TC-81-20 on line 8E to cover an up-ice direction from hole //19 of 1,250 ft. and north-northwest of hole TC-81-14 covering an up-ice distance of 2,350 ft. The drill area is contained by 7E to 21E; 18N to 37N. Drill hole locations are shown on Figure. 3.
The Heath k S herwood drilling equipment was mobilized from Kirkland Lake on Monday, August 23rd and demobilized on August 27th. Drilling of the 10 holes numbered TC-82-01 to 10 proceeded exceptionally smoothly with no problems or delays and production rate was 2 1/2 holes per actual drilling day. Equipment wear and used down-hole consumables was normal and adequately provided for in the budget.
A total footage of 1,575 ft. was completed of which 1,543 ft. consisted of
overburden for an average overburden depth of 154.3 ft. (Appendix A). A total of 30 ft. of bedrock, averaging 3 ft. per hole, was drilled. Bit production footage averaged 315 ft.
Figure l. LOCATION OF GOLDEIDT EXPLORATIONS INC.
MACKLEM S BOND TOWNSHIPS PROPERTY
ONTARIO \ QUEBEC
GO-.DEIDT PROPERTY , AWo, . SENNCTERREHORANDA
VKXTYN^viL D'Or l l
L. 4 E L8E L.12 E L.16 E
40 N
36ro ^,
*V
32 N —
P 23054 P 23C55
L.20E
1 V-N-/ ^V c ^ ?^r,Ja^pTcj^fl4^"'^. l;;'/!?'. /r:QTC-e2-03|\V-() 1 - s^-
T: i - J r ' T i p
28 r.-
24 \-
40N
36 N
32 N
20 N
16 N
-31 N
LEGEND
Intermediate metavolcanic
l l Mafic metavolcanic
Ultramafic metavolcanicIh
/
7x
TC-82-01
X Lithologic contact (assumed)
"s Ice flow direction
'S' Road
Marsh
Stream
Claim boundary
Reverse circjiotion rorory and numberTC-8I-I9 TC - 82-01
1981 series1982 senes
U. v\
DERRY, MICHENER, BOOTH S WAhil
GOLDEIDT EXPLORATIONS INC.
Macklerri S Bond Tps Pro,:ert^
LOCATION OF REVERSE CIRCULATION ROTARY DRILL HOLES
SEPT.y 1982 R. ROUTj.EDG^JFigure^^^
Forty-six overburden samples were collected from the lower 50 It. of glacio fluvial sediment and till in each hole. Glaciofluvial material was collected at plus or minus 5 to 10 ft. intervals whereas till or basal overburden was collected at less than or equal to 5 ft. intervals. Samples were shipped b bus to the Overburden Drilling Management Ltd. Laboratory in Nepean, Ontario for processing to heavy mineral concentrate. Three-quarter splits of heavy mineral concentrates were anal yzed for gold using the fire assay and atomic absorption method with minimum detection method of 5 ppb at Bondar-Clegg A; Company Ltd. of Ottawa. Minus 10 mesh bedrock cuttings were geochemically analyzed for Au, Ag, As, Cu, Ni, Pb and Zn by Technical Services Laboratories of Mississauga, Ontario.
R.E. Routledge of DMBW conducted binocular microscope examinations of bed- r'ock chips and anomalous heavy mineral concentrates.
Table l summarized the drill programme and a flow sheet illustrating labora tory sample processing is outlined in Figure k .
OVERBURDEN DRILLING THEORY, TECHNIQUE AND EQUIPMENT
Theory
In theory, subcropping concentrations of economic minerals were abraided or plucked and together with barren bedrock were incorporated within basal ice during the southerly advance of the Wisconsinan continental ice mass. This material was subsequently deposited as till from the moving sole of the glacier or transported englacially. Englacial debris was later released as terminal moraine at the glacier snout, when rates 'of wasting and advance at the ice-front were equal, or this debris melted out of the ice as supraglacial material or ablation till after stagnation of the ice mass during recession. This material was washed or flowed off the margin of the ice into pro-glacial lake Ojibway. Much of this debris was flushed from the glacier in glaciofluvial streams which formed eskers and esker deltas.
Ore minerals as discrete clasts or as constituents of rock fragments were dis persed and underwent cornmunition during transport to be deposited as constituents of till called dispersal trains. The outline of these trains within a till sheet is generally a cone which expands vertically and laterally within a till sheet as dis tance from the parent source increases. Dispersal trains are narrow and of limited length but possess areal dimensions many times larger than the subcrop area of the parent deposit. As an exploration target, this large size of the dispersal train increases the probability of discovery of the orebody.
Depending upon local glacial history, till may have been subsequently subjected to additional transport by succeeding glacial advances or ice margin fluctuations or reworked and deposited as glaciofluvial sediments. Therefore, either initial or resor ted dispersal trains may occur at any stratigraphic position and to optimize drift exploration the entire overburden profile is sampled. Correct interpretation of the overburden stratigraphy, depositional environment and sequence of glacial events is essential in determining the significance of geochemical and heavy mineral anomalies and tracing these anomalies to source.
COLPI::' EXPLORAT:C'JS INC.KdcHem f c 3on3 To^siips Property
5u"*vary of C.fSuraen Qr'lljng
A.:.st 21-27. :932
,
'.0.
:?
34
3
6
7
S
910
;
2i,23-;-:
:;^4
; ;2c.
26
25,25
ate
:i.'S2re/32
:i. 32:3 32:3. 52:3,32
ra/32Co/32rs/32ra/32
Location
8E/26+65N
8E/23+70NSE/sor?^:-!SE/32.7CN
16 *7SE;22.80N12EX30*rON
13+COC/-9N
15EX26t7CN19+70E/20N
(Ft.)
*8+ 13
-26 -18 14*4-6-21
FCC-.J:O.D.
o-:;fo-:;:;0-1:2o-:::.
o-:s:0-145o-i-:: iO-Kt0-14;
:- DrilledBedrcct
145-15C131J-192172-17:
104J-i:C
161-166146-147
161J-165176-177141-143
Dtp:-
15C19217711C
165147
165177143
S3~oles0.3,
6S :-
325
134
C:! lected3edrocl Bit No. /i
1 KC004311 ' K0004311 B634301 3634301 363431 1 B63432"1 3634311 3634311 KC004131 B63430
Cons'.-:Ftqe :
150382177237460 166312165177430
:'es
•^. '.o./i
11
2 22221
'i Ftcc
150382559669637 803489342177812
Reds
l Head Rod
j-jper fei/ 2.CCO (L!
ll l
i,:;: 32 1,57; ;o
Dr-lling order - holes l to 4, 10 to 7, O ;"d 6. rjjitionj! footo?e renains on bit. ,'sel head rgd.
Average bit life (4 bits) 3621'.
t 250g STORE
STORE
Light Fraction Pan samples
with abundant gold
Light Store
Bodrock Sample 1-5 kg
-10 mesh
+ 10 mesh
Binocular Microscc examination of eh i by DMBW.
Reject
Ship to Technical Services Lab. - analyse for Au,Ag,As,
Cu,Ni,Pb,Zn.Shaking Table
: Gold Grain Count
C j no Au k residu.il
Light Fraction STORE Heavy Liquid Separation
( M',1 thy lone; Iodide MG 3-3)
Magnetic Fraction
Ship to DMBW S Store'
1/4 - ship to DMBW Binocular Microscope Examination of Anomalous Concentrates and Store
Separation
-J So l i t
T3A Ship to
Bondar-Clegg 6 Co. Analytical Laboratory - analyse for Au
Figure 4 - Sample processing flov; sheet
Technique
The dual tube reverse circulation rotary technique is designed to deliver uncon solidated material continuously while drilling through the overburden and this permits logging and interpretation of the overburden stratigraphy and uninterrupted geo chemical sampling. Bedrock can also be drilled and rock chips collected, examined and analyzed.
Heavy mineral separates are prepared from bulk 5 to 7 kg overburden samples in order to concentrate weakly dispersed heavy minerals and amplify anomalies. Processing the sample in this manner effectively eliminates the "nugget effect" whereby a single or few significant ore grains are either lost in reject splits or report in retained splits to augment or "salt" the content of the analyzed reduced portion of normally processed geochemical sample. Concentration therefore retains all heavy ore minerals and is well suited to sampling immature, poorly sorted glaciofluvial sediments and tills having varied heavy mineral suites. Glaciolacustrine sediments other than beach facies are characterized by uniform suites of mainly non-opaque and non-ore heavy minerals and the source of any glaciolacustrine anomalies is virtually untraceable. Hence, glaciofluvial sediments and tills are cus tomarily logged and sampled whereas glaciolacustrine sediments are only logged.
Equipment
The Heath la S herwood drill employed on this programme was a unitizied rig consisting of a fully hydraulic Aker Drill with 10 ft. feed and ancilliary equipment such as a "Bean" piston water pump and air compressor mounted on a GO Track FT 3000 tracked carrier. A smaller Go Track GT-1000 on which a 500 gallon tank is mounted, was used to supply water to the drill rig.
A mixture of water, under high pressure and a capacity of 20 gallons per minute, and compressed air up to 60 psi is delivered to the 3 inch tri-cone bit face through the annulus between the inner tube and the outer wall of the dual tube rods (2.75 inches diameter). A slurry of cutting and material less than 1/2" dia meter is returned to surface'through the inner tube and collected from the cyclone where it is logged and sampled. Material is screened initially through No. 12 Tyler (10 mesh -1.7mm) sieve and collected in 5 gallon pails. The -10 mesh sample, including fines collected in an additional overflow bucket, are sampled. The + 10 m materials retained on the screens are logged and generally discarded unless base or precious metal mineralization is observed where upon the"oversize" is sampled separately and submitted for geochemical analysis.
GEOLOGY
BEDROCK GEOLOGY
Regional mapping by the Ontario Ministry of Natural Resources and Ontario Geological Survey is published in Pyke and others (1973) and Leahy (1971). Geology, previous exploration and gold mining potential of the Goldeidt property is available in detail in Routledge and Thompson (1982) filed with the Ontario Securities Commission.
The drill area is located in the northeast portion of the Goldeidt property and underlying bedrock is known only from reverse circulation drilling bedrock intersec tions and interpretation from regional aeromagnetic surveys and recently completed ground proton procession magnetometer surveys. Regional mapping indicates the area is underlain by calc-alkaline and tholeiitic volcanics.
Bedrock underlying the drill area is composed of equigranular, massive to foliated, light apple green to dark green, intermediate to mafic metavolcanic flows. Lithologic composition, on the basis of field identification, varies from andesite through andesite/basalt to altered (weathered) andesite or basalt and possibly to basaltic komatiite, From the evidence of "boulders" or slabs of identical composi tion drilled adjacent to bedrock and intersection of clay and sand-gravel filled seams, bedrock appears to be weather, fractured and broker at surface.
Because of the deep overburden obscuring bedrock and the presence of a mag netically interpreted north-south fault on the west side of the drill area, the widths and structure of these volcanic flows cannot be resolved with any degree of con fidence. Maximum thickness of the individual flow units, determined from the hole spacings, may be in the order of 300 ft. and likely considerably less.
Thin, 3 to 5 mm clear, barren quartz veinlets, mostly composed of sugary euhedral grains, and to a lesser extent carbonate veinlets are present in much of the bedrock as thin joint/fracture or foliation fillings. Very little carbonate altera tion of the volcanics has occurred. Limonitic surface weathering, possibly derived from the oxidation of minor pyrite, was observed in holes k a nd 9. No sulphide, gold indicator or gangue minerals were identified in rock chips obtained from dril ling.
Descriptions of bedrock chips and geochemical analysis of -10 mesh rock samples are listed in Appendices B.
QUATERNARY GEOLOGY1 V^ '"' ~ -- 1
Chernis and Averill (1982) on the basis of 30 wide spaced holes interpreted the glacial history. They postulate repeated Wisconsinan glaciations each of which eroded previous glacial materials and deposited till. Successive recessions were accompanied by the inundation of the glaciated area by lake Ojibway and deposition of glaciolacustrine sediments.
From bedrock to surface, Chernis and Averill subdivide the glacial stratigraphy into: a lower (lodgement) sandy till, lower deglacial sediments comprising grey silts and clays, a middle clayey till succeeded by an upper cobbly sandy till. This "stacked" till succession is overlain by upper deglacial sediments of esker sands and gravels and lake silts and clays. From the drill cross-sections, it is evident that complete sequence of stacked tills is preserved only on the flanks of the Fredrick- house esker, which overlies the east-central portion of the property and the 1982 drill area. Drilling elsewhere in this region (Routledge et al, 1981) has shown that glaciofluvial esker stratigraphy beneath glaciolacustrine sand aprons flanking eskers can be complex in that rhythmic sequences of the fluvatile coarse to fine elastics and clays can resemble unsorted tills as returned in drill slurries and hence be seen as indicative of episodic glacial advances. The correct genetic interpretation is critical in predicting transport distances of dispersal trains in till or eskers and in following-up gold anomalies.
GLACIAL, SJRATIQRAPHY
Glacial sediments of the drill area are considered to be Wisconsinan age (recession 6,000-8,000 B.P.) and are classified according to origin into major glacial units such as glaciolacustrine (gl), glaciofluvial (gf), and basal or lodgement till (BT).
Gray, lake bottom varved clays, oxidizing to yellow-brown at surface, and esker flanking apron sediments such as coarse to granular beach sand or lag gravel at surface, and very fine to fine sand at depth compose glaciolacustrine sediments (gl) which extend from surface to 100 ft. to 145 ft. Clay and silt at thicknesses of 12 ft. to 27 ft. underlie and interfinger with glaciofluvial materials in holes l, 2, 3, 6 and 10.
Glaciofluvial esker material (gf) in general was deposited earlier than glacio lacustrine units and consists of well sorted coarse to medium sand, pebbly and granular sand, and cobbly to bouldery gravel composed largely of Archean metavol- canic, Terniskaming metasedimentary and lesser felsic intrusive rock types typical of the Porcupine camp. Thinly bedded rhythmic sequences of interbedded gravel, sand and silt or clay characteristic of esker delta sedimentation are further subdivided into unit (gfr). This occurs as a transition unit up to 14 ft. thick between glacio fluvial (gf) and glaciolacustrine (gl) sediments.
A green, pebbly to bouldery gravel unit, up to 14 ft. thick, termed "green diamicton" (dt) is so named because of abundant green clay rock flour produced from drilling altered mafic to ultramafic volcanic boulders and cobbles, likely derived from the ultramafic bedrock, laying to he north on Asarco property. The diamicton is distinguished from true till by properties such as bedding, rounding of clasts, good sorting of coarse to medium sand matrix and by correlation to glaciofluvial and glaciolacustrine units between holes which suggests that this unit is more likely related to esker sedimentation rather than the alternative interpretation of till deposition during a limited ice margin fluctuation in this area. This till-like unit could also have originated from flushes of supraglacial debris or melt-out material from the base of lifting or floating ice at the ice margin, i.e. turbidite.
From 3 ft. to 14 ft. of basal till was identified in holes 2, 3 and 8 and pos sibly occurs in washed or reworked form in holes 6, 9 and 10. Till is identified by poorly sorted fine to medium gray to green and, green rock flour and grey clay-silt matrix and angular volcanic-sedimentary rock fragments in addition to rounded clasts of local bedrock debris-boulder content. Lack of bedding, mix of rock fragments and pebble shapes and nature of clay-silt component are main criteria for distinguis hing the till from units of flaciofluvial, rhythmite and green diamicton material. - Washed till (btw) lacks fines such as clay and silt and shows some sorting of sand matrix but rock fragment and pebble lithology and lack of bedding in addition to basal stratigraphic position suggest that fines have been washed and it is a reworked till. At higher elevations till may not haVe been deposited or alternatively, late- stage subglacial esker streams may have eroded to bedrock and removed till, or have action from low lake levels may have washed till from bedrock at higher elevations.
BIBLIOGRAPHY
Chernis, J. and Averill, S.A.1981: Goldeidt Explorations Incorporated, Macklem Township, Porcupine
Mining Division, Ontario - Reverse circulation drilling report; M.N.R. Assess. File Rept., 33 pp.
T
Leahy, E.J.1969: Macklem Township, District of Cochrane; O.D.M. Prelim. Geol. Map
P. 546, scale 1:15,840.
1971: Geology of the Night Hawk Lake area, District of Cochrane; Ontario Dept. Mines and Northern Affairs, Geol. Rept. 96,74 pp, map 2222, scale 1:31,680.
Leahy, EJ. and Hogg, D.W.1962: Preliminary geological map - Rond Township; O.D.M. Map No. P161,
scale 1:15,840.
Lee, Hulbert A.1968: An' Ontario kimberlite occurrence discovered by applicator) of the
glaciofocus method to a study of the Munro Esker; Geol. Suvey of Canada, Paper 68-7, 3p.
Pyke, D.R., Ayres, L.D., and Innes, D.G.1973: Timmins-Kirkland Lake Geological Compilation Series, Cochrane,
Sudbury and Timiskaming Districts; Ontario Div. Mines Map 2205, scale 1:253,440.
Routledge, R.E., Thomson, I., Thompson, I.S., and Dixon, J.A.1982: Report on 1982 Reverse Ciruclation Rotary Overburden Drilling
Programme - Mackline Township, Goldeidt Explorations Inc.
Routledge, R.E. and Thompson, l.S. (Derry, Michener, Booth (5c Wahl)1982: Report on Macklem and Bond Townships Property Timmins, Ontario
of Goldeidt Explorations Inc.; Ontario Securities Commission Rept., 45p.
APPENDIX A
OVERBURDEN DRILL LOGS
HEVERSE
DATE AHOLU
GEOLOGIST
LOCATION
^
SHIFT MOVE TO HOLE // ;3O — /S'37
DRILL __l*Sutr
HIT
for
CLIENT: Go(e(e*
BIT ROOTAGE JB.
So
TOTAL HOURS MECHANICAL DOWN TIME
DRILLING PROBLEMS -—-
CONTRACT HOURS OTHER
MOVE TO NEXT HOLE
EL e if A TiPA/ : O '- et* tu M
~ /S'-
u
GRAPHIC LOG
SAMPLE NO.
DESCRIPTIVE LOG
Motes l Analyses
'O -
JO -
50-
10-
'-'i
- s 's ' —'"x"
orJt*t
V
(r
fa
f~0
*y-y hSW
f Hoi- .No. l Page '
HOLE HO -4L LOCATION .DRILLER BIT NO
CLIEfJT: JUIT POQTAGE
MOVE TO HOLE
DRILL .——————
TOTAL H OURS
CONTRACT HOURS
MECHANICAL DOWN TIME
DRILLING PROBLEMS ™-
OTHER ——...-.-,—————-
MOVE TO N EXT HOLE,
C
DESCRIPTIVE LOG
Notes a Analysesp?"*
c* M PI 7*
no H
/SD-
03
oS
*
fame,
S***"* f -f l
S f*
Hi
V-** litftt St^ff tf
w/Vi'
6W
130
75"
10
77 O
lo SB
FMC'
^
REVERSE CIRCULATION DRILL HOI.P LOG
li II ^ li
SHIFTjftjo TO //-#
HOLE NO./.C-
GEOLOGISlXL/^
MOVE TO HOLE
DRILL ____Z
.L-PJL- LOCATION .A
l D RILLER
'*SV - t
Bl r
-f^ CLIENT:
BIT FOOTAGE
- s otfsTOTAL HOURS
CONTRACT HOURS
MECHANICAL DOWN TIME
DRILLING PROBLEMS —^.
OTHER ———-—-————.
MOVE TO /?o*D /O'-SS-SS:3v
LJ LJU.
GRAPHIC LOG
SAMPLE NO.
DESCRIPTIVE LOG
Notes S Analyses
J-P -
/o-
1 1 1f
' x x x't'x
X/X '
fo-
/**
'/'x/X/'/X
. ' . 0~\ ' "
erntHi\e*(
U
0
f*i"r
f*
REVERSE CIRCULATION DRILL HOLE LOG
DATF?? / K e,"M fi
TO
HOLE WO..^^-™,——
GEOLOGIST /f^^/V^ti DRILLER
MOVE TO HOLE i______________
DRILL __________________———
BIT NO. BIT FOOTAGE
TOTAL HOURS
CONTRACT HOURS
MECHANICAL DOWN TIME
DRILLING PROBLEMS ——
OTHER ™———..-—-——
MOVE TO NEXT HOLE
0
a o
SAMPLE
NO DESCRIPTIVE LOGfi*
A,Notes S Analvses
Cu.M' fi
//H
.0
•oo- o-|6•080
Ifo-
o/
03
fy*y
V
itwr-
a
^ —— ̂
/lyl'-
US?
2 SO
12 O.V 33
: ; cio No. j "Page
"""9 J l J? J
SHIFT
•ICLH NO. TC - g;?. - flgGEOLOCMST ^ ̂ Dufif^a DRILLER
MOVE TO HOLE /2~V8 ~ /2-ff
DRILL /2 : SJ~ /8--&0 A /f S*
W^ CLIENT: G t&M 6/6 f*.
BIT HP /f 400 #XJ HIT FOOTAGc. g ~ /??
S*f
TOTAL H OURS
CONTRACT HOURS
MECHANICAL DOWN TIME
DRILLING PROBLEMS ™-.
OTHER -^-
MOVE TO NEXT HOLE H /O
foils f o 8 ! O 5 "
UJ Ul
GRAPHIC LOG
SAMPLE NO.
DESCRIPTIVE LOG
Notes a Analyses
c*.PP.*.
f- t
777. / -fi.
to-*
/ ' x1 x -l' 1
'2\
r! r
0- l
W**-
**~t
.
OUtifl&tf
-/t t
A
AAr-tr ^*-*
fas
c4**-t
Ho i e No. r ?,':.-
DATE 19HOLE "
-
—— B.T no. .OOTAGE
SHIFT
TOTAL H OURS
MOVE TO HOLE
DRILL ———————
CONTRACT HOURS
MECHANICAL DOWN TIME
DRILLING PROBLEMS .———
OTHER _____———————
MOVE TO NEXT HOLE,
Ul UJ UL
GRAPHIC LOG
SAMPLE NO.
DESCRIPTIVE LOG
tp* a Analyses
A* uff m-M-
In
110 -j
/20-4
139.
i.*
/fff-
JJTot t 5w
3Tc?*-|tot)
'0.-OV^•^
O-".9
/^H
s
01
o^
06
i
H
y*
li/o
l f 3'^
/i?'- /6?'/*
/?o' ^
/^/' ^
1 ? -5"
9/6'
13 0-3 st- St 12
Hole No. |-?a^
HEVhHbt-
- 191*l OCAT.OM LL
B,T NO.
CLIEfff I
BIT FOOTAGE
SHIFT MOVE TO HOLE
DRILL ff 8
TOTAL H OURS MECHANICAL DOWN TIME
———-— DRILLING PROBLEMS
CONTRACT HOURS O THERMOVE TO NEXT HOLE
St-
Notes l Analyses
HOLE
SHIFT 4)______TO^.
%2-JJL. I OCAT.OM f S.*!tel/**™*- CLIENT: d1GEO;OG,s72^^0R, l.L ER A^WJ- B,T NO.——————— BIT FOOTAGE
MOVE TO HOLE
DRILL —————-—
TOTAL H OURS
CONTRACT HOURS
MECHANICAL DOWN TIME DRILLING PROBLEMSOTHERMOVE TO NEXT HOLE
APPENDIX B
BINOCULAR DESCRIPTION OF BEDROCK CHIP SAMPLES
TC-82-01-07 Dark greenish-grey, chloritic, very fine-grained equigranular mafic metavolcanic of basalt composition. Slight carbonate alteration of weakly foliated matrix. Thin veinlets of clear quartz and coarsely crystalline calcite 3 to 5 mm thick.
TC-82-06-04 Dark greenish-grey very fine-grained equigranula mafic metavolcanic of basaltic or basaltic komatiite composition. Abundant 4 to 5 mm thick barren, clear quartz veinlets.
TC-82-09-11 Medium greenish-grey, well foliated, chloritic intermediate to mafic metavolcanic. Felty equiangular matrix with less than 596 amphibole (actinolite) porphyroblasts retrograde-altered to chlorite.
TC-82-10-05 Light greenish-grey, aphanitic, intermediate metavolcanic. Amphibole (actinolite or hornblende) occurs as porphyroblasts less than 1/2 mm, discontinuous streaks and banding developed parallel to weak foliaton. Andesite composition.
Ministry of ,- Natural
Ontario
Report of Work(Geophysical, Geological, Geochemical and Expenditures)
Instructions: - Please type or print.— If number of mining claims traversed
exceeds space on this form, attach a list. Note: - Only days credits calculated in the
",'Expenditures" section may be entered
The MinirType of S urvoy(s)
o Citew c /HClaim Holder(s)
(t* (; f?- fa
900Address
fi O. I^Survey Company
Name and Address of Author (of Geo-Technical report)
Date of Survey (from Si to) ^,3./, icj e.2\ 2~i v e'2,Day l Mo, J Yr. j Day | Mo. | Yr.
Total Miles of line Cut
O
Credits Requested per Each Claim in Columns at right Mining Claims Traversed (List in numerical sequence)Special Provisions
For first survey:Enter 40 days. (This includes line cutting)
For each additional survey: using the same grid:
Enter 20 days (for each)
Man Days
Complete reverse side and enter total(s) here
Airborne Credits
Note: Special provisions credits do not apply to Airborne Surveys.
Geophysical
- Electromagnetic
- Magnetometer
- Radiometric
- Other
Geological
Geochemical
Geophysical
- Electromagnet
- Magnetometer
- Radiometric
- Other
Geological
Geochemical
ic
Electromagnetic
Magnetometer
Radiometric
Days per Claim
Days per Claim
Days per Claim
Expenditures (excludes power stripping)Type of Work Performed , x i ,, /'
Performed on Claim(s) "
Calc ulation of Expenditure Days Credits
Total Expenditures
S 1 &, / /V.J2 y -H 15
c
(ffiTT
A7
Total )ays Credits
loot:Instructions
Total Days Credits may be apportioned at the claim holder's choice. Enter number of days credits per claim selected in columns at right.
p;
)
M.
Mining ClaimPrefix
-
RCUPINE Wt? (ft ffc, p IE
MAY 2
Number
&V rx,t
;A^CJ3
NING OIVI5IOHn n n r. J r^T\
3 li u UJ 111
P.M.2|1|?|3|^5|V.
Expend. Days Cr.
p**bA,:-
1
-1 R
;wo
"I
For Office Use OnlyTotal Days Cr. Recorded
Date Recorded 1 "l)i. . - 1 J i j 2
Mining ClaimPrefix
RE'
INING
mm
41NG l
; c oMAY 5oiKO. ..
Number
-PlVH^Cl V En*
f 1 8 1983
LANDS SECT
|E1VEP3 1 1983...~r ccrtic
tf^ \ ™ *^ ̂
1
R. D li D
Expend.Days Cr.
}
ON —
JN
Total number of mining claims covered by this \ \ \~ report of work. O*- O
*tctuf*'t-te^jZ&r*/ i
Date fc4ificatiori
n Reeprdeb Holder or Agent (Signature) i|\ A i1 --*. \
Certification Verifying Report of Workl hereby certify that l have a personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report is true.
Name and Postal'Address of Person Certifying l } C -. N- , l___JX^-S t IrxiA-Uu
i .M "7 LYN b /\\ r' oDate Certified i i^J ,, , , :-7/
Certified by (Signature) If' \ . .-*-f
CLAIM NOS.
P529045529046529047529048529049529050529051529052529053 '529054529055529056529057529058529059529060529061529062529063529064529065529066529067529068529069
Expenditure Days Credit: 40.*k days/claim
Our File: HMW54"
February 16, 1984.
Goldeldt Explorations Inc.P.O. Box 36Toronto Dominion CentreToronto, OntarioM5K 165
Attention; R. Sibthorpe
Dear Sir:
RE: Reverse Circulation Overburden Drilling data submitted on Mining Claims P 529045 et al In the Township of Macklem., . --- ------.
We have not received receipts or cancelled cheques required In order to assess work performed on Mining Claims listed above. Please provide receipts verifying payment of the expenditure ofSI5,114.24 for Overburden Drilling.as soon as possible.
Yours very truly,
J. R. MortonActing DirectorLand Management Branch
Whitney BlockRoom 6643Queen's ParkToronto, OntarioM7A 1W3Phone: (416) 965-1380
M. t . Anderson:dg
cc: Mining Recorder Timmins, Ontario.
anagement Branch 'if.:. ! ' i /".is Q]
RECEIVED
LANDS SECYIOP
THETOBOhtTG-DOlVliNiOTORONTO-DOMINION CENTRE BR. ; 55 KING ST. W. b B AY STREET TORONTO, ONT. M5K IA2
^- a
PAY 'l O l ML Of
i: io;oj'"00i,i: DE,Vi
FO
R D
EPO
SIT
ON
LYT
O T
HE
CR
ED
IT O
F
HEA
TH S
t SH
ERW
OO
D D
RILL
ING
D/V/
5/OW
OF
Eiia:.;
;.,^R
H;.::G
:;AL S
ERVICE
S LTD
.
telephone 4\6-S64-730\ (•le* 06-22627
Gold
luile 90S, 40 university avenue,
Goldeidt Exploration Inc., to 19th Floor, Midland Doherty Ltd.,
Commercial Union Tower, Toronto Dominion Centre, Toronto, Ontario. M5K IBS.
toronto, Ontario, September 2nd, 1982M5J 1T1
Invoice No. 9797D.O. 448Project No. 82-057
in account with
heath 8t sherwood drillingdiviiion o' challenger international lervicei ltd.
terms: net coih 1 S d ayi after dale of Invoke
hole no.
TC-82-01
TC-82-02
TC-82-03
TC-82-04
TC-82-10
TC-82-09
TC-82-08
TC-82-07
TC-82-06
e. i o. e.
to cover diamond drilling
from to
for the period
footage completed
Drilling program on the townships of Makem and Province of Ontario. - August 23rd-27th,1982
rate
Bond in the
Mobilization and DemobilizationLump Sum Moving in from end of truck road to fist hole 1 Moving from last hole to end of truck road
Reverse circulation rotary drilling0 150
Rig Hours
0 190 Rig Hours
0 177 Rig Hours
0 110 Rig Hours
0 143 Rig Hours
0 177 Rig Hours
0 165 Rig Hours
0 147 Rig Hours
0 148 Rig Hours
150 2.75
190 10
177 3.5
110 2.25
143 4.75
1776.5
165 3.75
147 2.25
148 3.25
.5 rig hrs
.5 rig hrs
2.50 139.25
2.50 139.25
2.50 139.25
2.50 139.25
2.50 139.25
2.50 139.25
2.50 139.25
2.50 139.25
2.50 139.25
139.25
139.25
375.00 382.94
475.00 1,392.50
442.50 487.38
275.00 313.31
357.50 661.44
442.50 905.13
412.50 522.19
367.50 313.31
370.00 452.56
250
208
69
757
1,867
929
588
1,018
1,347
934
680
822
.00
.80
.63
.94
.50
.88
.31
.94
.63
.69
P 81
.56
telephone 416-364-7301 (•let 06-22627
tyite 908, 40 university ovenue,
to
toronto, ontorio, S eptember 2nd , 1982M5J IT)
Invoice No. 9797Page -2-
in occounl with
heath a sherwood drillingdiviiion of challenger international services ltd.
terms: net cosh 1 5 days after dale of Invoke
hole no.
T-82-06
e. i o. e.
to cover diamond drilling for the period
from to footage completed rate
0 166 166 2.50 415.00Rig Hours 3
Travel Time in excess of oneAug. 24thAug. 25th
m
l
Rig ServiceAug. 24th
26th27th
.Material consumed2-15/16" reverse circulationbutton bits 5Bit Nos. K-000431, B-63430,K-000413, B-63431, B063432
2-15/16" dual tube rodbit subs 2
2-15/16" dual tube starterhead rod 1
Super Poly 2000 9
Plus il.5%
139.25 417.75
hour per shift25 rig hrs.25 rig hrs.5 rig hrs @ 3 men or.5 man hrs. 20.00
25 rig hrs.252575 rig hrs. 124.65
only 675.00 3,375.00
only 262.00 524.00
only 250.00
Litres 7.50 67.504,216.50
632.48
Wfe
832
30
93
4,848
$15,281
.75
.00
.49
98A99 y//
Ministryof GeotechnicalRNea:is Report
Ontario W Approval
File
xss y
Mining Lands Comments U
o: Geophysics
Comments
l l Approved | ] Wish to see again with correctionsDate Signature
To: Geology- Expenditures
Comments
[~] A pproved l Wish to see again with correctionsDate Signature
To: Geochemistry
Comments
^Approved [ j Wish to see again with correctionsDate
To: Mining Lands Section, Room 6462, Whitney Block. (Tel: 5-1380)
1593 (81/10)
May 30, 1983 2.5554
Mr. WU 11am L. GoodMining RecorderMinistry of Natural Resources60 Wilson AvenueTimmins, OntarioP4N 2S7
Dear Sir:
We have received data for Reverse Circulation Overburden Drilling of the Mining Act. R.S.O. 1980 for Mining Claims P529045 et al 1n the Township of Macklem.
This material will be examined and assessed and a statement of assessment work credits will be Issued.
We do not have a copy of the report of work which Is normally filed by you prior to the submission of this technical data.
Please forward a copy as soon as possible.
Yours very truly,
E.F. AndersonDirectorLand Management Branch
Whitney Block, Room 6450Queen's ParkToronto, OntarioM7A 1W3Phone: 416/965-1380
A. Barr:mc
cc: Goldeldt Explorations Inc. P.O. Box 36
Toronto Dominion Centre Toronto, Ontario M5K IBSAttention: R. Sibthorpe
