23
41N15NEeei2 2 ,13693 MCMURRAY 010 2.13693 CITADEL GOLD MINES, INC. REPORT ON GEOLOGICAL MAPPING SOUTH PART OF BLOCK "A" AT DEEP LAKE MINE WAWA, ONTARIO RUSSELL G. REID 1990-10-10 DEEPLK.GEO
41N15NEeei2 2 ,13693 MCMURRAY 010
2.13693
CITADEL GOLD MINES, INC.
REPORT ON GEOLOGICAL MAPPING
SOUTH PART OF BLOCK "A" AT DEEP LAKE MINE
WAWA, ONTARIO RUSSELL G. REID 1990-10-10
DEEPLK.GEO
4!N15NEeai2 2 .13693 MCMURRAY
TABLE OF CONTENTS
SUMMARY AND CONCLUSIONS
INTRODUCTION
PROPERTY OWNERSHIP, LOCATION AND ACCESS
HISTORY
GENERAL GEOLOGY
PROPERTY GEOLOGY
STRUCTURE
MINERALIZATION
REFERENCES
APPENDIX I - ASSAY RESULTS
LIST OF FIGURES
PROPERTY LOCATION PLAN
SCHEMATIC OF DEEP LAKE MINE AREA
GEOLOGY PLAN #3-4.. . . . . . . . . . . . . . . , . . . . . . . . . . . . . . . . . ..Back Pocket
DEEPLK.GEO
CITADEL GOLD MINES INC. REPORT ON GEOLOGICAL MAPPING
SOUTH PART OF BLOCK "A" AT DEEP LAKE MINE
SUMMARY AND CONCLUSIONS
Geological mapping was concocted on a grid cut in December of 1988 and March of i989 on a block of 5 contiguous claims owned by Citadel Gold Mines, Inc. The mapping was completed during September and October of 1990,
The Deep Lake claims are mainly underlain by intermediate volcanic flows and pyroclastics. The majority of the volcanic rocks show a pervasive silicification with little to no associated sulphide mineralization. The rocks are generally massive with little foliation developed, and only local shearing noted proximal to some topographic depressions.
Where observed, the regional foliation trend is easterly to northeasterly. A rotation towards the direction of major northeast-southwest trending lineaments indicates some ductile fault movement along the lineaments. The geometry and relative change in orientation of the quartz vein hosting the Deep Lake Mine as the vein approaches the gully south of the shaft indicates a sinistral sense of movement along that lineament.
Rusty gossan zones occur in numerous locations throughout the property, usually proximal to flow contacts. Sulphide content, (less than 1056) is dominantly fine grained euhedral pyrite disseminated throughout, occasionally on fracture planes. Pyrrhotite, in smaller percentages was observed, as well as occasional chalcopyrite in the larger gossan zones. These zones were the focus of much of the early trenching in the area.
Significant recorded gold mineralization on the property is confined to the Deep Lake Mine vein, and is only reported visible on surface at the gully south 0f the shaft. This location has been covered by waste rock from the mine. Given an apparent sinistral sense of ductile movement along the northeast trending lineament, the quartz vein would have experienced dilation as it intersected the shear/fault zone. This allowed for the gold mineralization to concentrate. Current assay results from the vein range from trace to 0.012 ounce gold per ton.
Based on observations made during the current geological mapping program, further detailed prospecting of the known quartz veins on the entire Citadel Block "A" Property is warranted. An emphasis should be directed to the areas where they intersect major lineaments or show a dilatent character (noteably chloritic partings perpendicular to the strike of the vein observed proximal to the Deep Lake Mine) and minor rotations of the strike direction, /? S
DEEPLK.GEO
INTRODUCTION
The 5 claims covered by this survey were staked by Citadel personnel in January 1988. Linecutting and a ground magnetic survey was conducted in the winte|r of 1988-89 to provide a basis for geological mappping, prospecting and possible diamond drilling in this area.
Geological mapping was performed by the author under the employ of Citadel Gold Mine, Inc. The work was done in September and October of 1990.
PROPERTY OWNERSHIP, LOCATION AND [ACCESS
The property consists of 5 v^npatented mining claims owned by Citadel Gold Mines, Inc. They are numbered as follows:
SSM 937795 SSM 937796 SSM 937797 SSM 937798 SSM 937799
Surface rights to the claims are retained by the Crown.
The attached location plan (Figure 1) shows location of the claims, and indexes the individual map sheets.
The property is located in the central part of McMurray Township in the District of Algoma and the Sault Ste. Marie Mining Division. It is about thi'ee miles southeast of the Town of Wawa and may be reached vi^ the Deep Lake Mine Road which extends east from Surluga Road. The Deep Lake road is a cart track passable by four-wheel drive truck in good weather. The Surluga Road is a gravel surfaced road seasonally maintained by the municipality or by Citadel Gcjdd Mines Inc.
HISTORY
Previous work on this property consisted of intermittent poorly recorded prospecting since the late 1800's. In the 1930's, gold was discovered at the Deep Lake Mine where a small mill and refinery was constructed. Some gold was produced from the mine, and the 0wners reported gold output from the refinery in 1936, Nearby areas were prospected about this time, as evidenced by numerous debris-filled trenches on or near the claims.
In the late 1930's and again in the 1960's and 1970's, the Deep Lake Mine was repeatedly used by promoters to raise money, based on the published production of 1617 ounces of gold and 2790
DEEPLK.GEO
CITADEL OLD MINES INC. "OWNED by CITADEL
OPTIONED
FORMER PRODUCING MINES
tons of rock removed from the (line by the owners in 1936. This production was attributed by later promoters to the government agency which published these reports, and the reports do not state that all of the gold was derived from the Deep Lake Mine ore. These past operators resampled the mine in the late 1930's, and completed some stripping and about 7 poorly recorded drill holes in the 1960's and 1970's.
Surface trenching at the Deep Lake Mine and resampling of the vein in 1979 for Golden Goose Gold Mine Co. Ltd (Rupert, 1980) returned an average of 0.009 ounce per ton gold for 35 assays. The reported assay vjalues ranged from the minimum detection limit ^0.001) to 0.026 ounce per ton gold.
Geological mapping of the contiguous claims to the north was completed by personnel of Citadel Gold Mines, Inc. (Plackitt and Butorac, 1987).
Available reports include:
1) Report on Deep Lake Mine by R. D. Caylor, 1937.2) Closure plan of Deep Lake Mine, Hesse, 1938.3) Drill Logs, assessment work files, Paul McLean, 1964.4) Sampling Report for Golden Goose Ltd., Rupert, 19805) Dighem for Citadel, 19866) O.D.M. Map P838, 1973.7) O.G.S. Map P2441, 1982.
GENERAL GEOLOGY
The property is underlain by Archean volcanic strata. ODM map P.838 indicates that most of the claims are underlain by felsic to intermediate volcanic strata intruded by a few dykes of diorite with a similar compostion. The Helikian Firesand Carbonatite is a 4000 foot diameter concentrically zoned alkalic intrusive, shown on OGS maps P.828 and P.2441 to be located about 3000 feet north of the east end of these claims.
The principle magnetic feature of the area is the Firesand Carbonatite and related lamprophyre dyke swarms which parallel its contacts, or fill narrow pre-existing fractures within several miles of the main plug. The Carbonatite Plug has high magnetic permeability, and creates a pronounced magnetic gradient across the claims. The peripheral narrow recessive dykes of lamprophyre up to 5 feet wide contain variable quantities of magnetite, up to 2056, and they crjeate numerous magnetic anomalies throughout the district. In the Surluga Mine, two miles west of the Firesand Carbonatite, these dykes comprise about 5 percent of the rock mass.
DEEPLK.GEO
WORK PROGRAM PARAMETERS:
Grab samples were taken for assay purposes randomly over the property. The geological mapping and sampling was controlled by use of a previously cut grid.' The Baseline and tie-line are oriented at an azimuth of 0250 with crosslines at 400 foot intervals (Az 1150 ). Total cut li,ne is 2.8 miles over the claims covered by the current survey. The shore of Deep Lake was mapped using a small rowboat and airphoto; enlargement for control.
PROPERTY GEOLOGY
The Deep Lake claims are principally underlain by intermediate volcanic flows and pyroclastics. The majority of the volcanic rocks show a pervasive silicification with little to no associated sulphide mineralization.
i
MAFIC VOLCANIC ROCKS
FLOW UNITS:Two areas of mafic volcanic} rocks were encountered during
the present survey, the larger being on L 16S near 22W, and another single outcrop at L 12S near 13W. These rocks are massive, fine to medium-grained of chloritic composition. These rocks may be fine grained gabbroic rocks, but no intrusive relationships were observed.
INTERMEDIATE VOLCANIC ROCKS
FLOW UNITS:Massive and porphyritic andesite flows underly the majority
of the claim group. PorphritiC Andesite is a predominantly comprised of 1-50?6 plagioclase phenocrysts ranging from 1/16" to 3/8" in diameter. Some units mapped as flows may be of tuffaceous origin. The matriit is fine to medium grained of intermediate composition. Local low grade metamorphism evidenced by biotization, chloritization and silicification are enhanced near the contacts of the pyroclastics. This characteristic is sometimes associated with lineaments of variable strikes within the north-south to northeast-southwest direction. Foliation features were rarely observed and maintained similar azimuths to the major lineaments.
VOLCANIC BRECCIA:This unit is comprised of fragments of porphyritic andesite
cemented by fine grained to aphanitic material of similar composition. The breccia occurs in close proximity to surrounding tuffaceous units. The Volcanic Breccias are of both pyroclastic and autoclastic origih. Some may also be altered flows which have been fractured as a result of movement along the major faults/lineaments.
DEEPLK.GEO
TUFFS:The tuffaceous units are maihly crystal and ash tuffs. They
maintain an intermediate andesitic composition with barely visible, well sorted crystals. Well sorted tuffs with plagioclase phenocrysts of up to 3mm are also present. Foliation features are poorly developed but where observed conform to the general strike direction of njortheast-southwest. Some of the plagioclase porphyritic flows may also be of tuffaceous origin.
FELSIC VOLCANIC ROCKS
PYROCLASTIC UNITS:Felsic volcanic rocks are comprised of crystal and lapilli
tuffs, quartz-eye tuffs and pyroclastic breccias. Within the eastern portions of the map area, they form a discontinuous east- northeast trending zone of dominantly crystal tuffs and tuff breccia. Felsic volcanic rocks are the principle unit underlying the area between the Deep Lake Mine and the shore of Deep Lake. Plagioclase phenocrysts up to Snirn comprise 30 to 50 percent of the rock with occasional quartz eyes, set in a fine grained to aphanitic ash matrix of felsic composition. The pyroclastic breccias are comprised of angular blocks of similar composition to the tuffs set in a felsic ash and crystal matrix.
FELSIC INTRUSIVE ROCKS
QUARTZ-FELDSPAR PORPHYRY:A massive porphyritic intrusion underlies the central
portion of claim SSM 937798, along the Baseline south of L 0. It is comprised of 20 to 4056 euhedral plagioclase phenocrysts, 3 to 5mm in size. Blue quartz eyes 3 to 6mm in diameter comprise 3 to 2096 of the rock. The intrusion is relatively leucocratic, containing an average of less than 5% mafic minerals, mostly biotite.
MAFIC INTRUSIVE ROCKS
GABBRO:A relatively large northwest trending gabbroic intrusion
underlies portions of the adjacent Van Ollie Explorations property {Butorac and Mills, 1990), and outcrops on the shore of Deep Lake. Where noted on claim SSM 937795, it is medium to coarse grained, hornblende rich ind equigranular. An area of high magnetic response defined by a previous magnetic survey (Rupert, 1989) under Deep Lake may represent an expansion of this mafic intrusion.
Other small gabbroic dykes occur on the property, and generally trend parallel to major lineaments, northeast- southwest.
DEEPLK.GEO
LAMPROPHYRE:A northeast trending lamprophyre dyke outcrops twice on the
shore of Deep Lake, It is a relatively incompetent, coarse grained biotitic rock with a thick weathering rind. This dyke continues northeasterly, and is reported to outcrop in the gully south of the Deep Lake Mine. Other lamprophyres may occupy northeast trending lineaments across the property.
STRUCTURE
The rocks underlying the Deep Lake property are generally massive with little foliation developed, and only local shearing noted proximal to some topographic depressions.
Where observed, the regional foliation trend is easterly to northeasterly, dipping moderately to the south. Some rotation towards the trend of major lineaments, noteably the gully trending southwest from the Deep Lake Mine area towards Deep Lake, indicates some ductile fault movement along this particular lineament. The geometry and relative change in orientation of the quartz vein hosting the Deep Lake Mine as it approaches the gully indicates a sinistral sense of movement along this lineament (see Figure 2). Chloritic partings oriented perpendicular to the contacts of the quartz vein also indicate some movement has occurred.
MINERALIZATION
A total of 21 rock assay sanjples were collected and analyzed during the current survey. The sample locations are shown on the surface geology plan (back pocket}), and assay results are listed in Appendix I.
Rusty gossan zones occur in numerous locations throughout the property, usually in close proximity to flow contact zones. Sulphide content, (less than 1 Q%) is dominantly fine grained euhedral pyrite disseminated throughout, occasionally on fracture planes. Pyrrhotite, in smaller percentages was observed, and occasional chalcopyrite in intensely gossanous zones. These zones were the focus of much of the early trenching in the area. No significant assay results were obtained from these units.
To date, significant gold mineralization on the property is confined to the vein at the Deep Lake Mine. Gold is only reported to be visible proximal to the gully near the shaft collar (Caylor, 1937). Given the structural relationship of a sinistral sense of ductile movement along the lineament south of the shaft, the quartz vein would have experienced dilation as it approached the sheir/fault zo/ne, allowing for the gold mineralization to concentrate in this area (see Figure 2).
DEEPLK.GEO
"
Figure 2. Schematic Structural Model of the Deep Lake Mine Area.
DEEPLK.GEO
•f
kAnomalous gold mineralization within the Deep Lake Mine vein
has been confirmed by the present survey, however a best result of 0.012 and 0.010 ounce gol^ per ton (Samples 4149 and 4156 respectively) is less than encouraging.
Respectfully tted
R.G. Reid Geologist
DEEPLK.GEO
REFERENCES
Butorac, S., Mills, P* and Varill&s, H. January, 1990. Geology of the Van Ollie Explorations Ltd. Property, Sault Ste, Marie Mining Division, Ontario. In Assessment Files, Wawa Resident Geologist Office. |
Caylor, R.D. March, 1937. Deep Lake Gold Mines Limited, Private Report to E.B. Gill, Esq. Unpublished Report, in Files of Citadel Gold Mines, Inc.
Hesse, 1938. Closure Plan of Deep Lake Mine. In Assessment Files, Wawa Resident Geologist Office.
Kilty, S.J., 1986. Dighem III Survey of the Wawa Area, Ontario Unpublished Report by Dighem Surveys and Processing for Citadel Gold Mines Inc., December 1987.
McLean, Paul, 1964. Diamond Drill Logs, various locations, McMurray Township. In Assessment Files, Wawa Resident Geologist Office.
Plackitt, A. and Butorac, S., Decjember 1987, Geology Plan, Block "A" Property (Deep Lake) for Citadel Gold Mines Inc. In Assessment Files, Wawa Resident Geologist Office.
Rupert, R.J., 1973. Geology of McMurray Township and parts of surrounding townships. O.D.M. Preliminary Map Number 828. Scale 1:15840
1980. Geological Sampling Report for Golden Goose Gold Mines Lts. on the Deep Lake Mining Property, Wawa, Ontario, In Assessment Files, Wawa Resident Geologist Office.
1989. Citadel Gold Mines Inc., Report on Magnetometer Survey, South part of Block "A" at Deep Lake Mine. In Assessment Files, Wawa Resident Geologists Office,
Sage, R.P., Sawitsky, E., Turner, J., Leeselleur, P. and Sagle, E., 1982: Precambrian Geology of McMurray Township, Wawa Area, Algoma District; Ontario Geological Survey Preliminary Map P,2441, Geological Series, Scale 1:15 840 or l inch to 1/4 mile. Geology 1979.
DEEPLK.GEO
;i*
APPENDJX I
Rock Assay Certificates
Sample Numbers
4136 4140 -i 4159
DEEPLK.GEO
-- V.^^K-.--^fs^nl
HiTEfeANAL^ig^- HAILEYBbRY. ONTARIO
QJ^irttflcate
0762
SAMPLE(S)OF: Rock
SAMPLE(S) FROM:
FAX:
DATE: September 25, 1990
RECEIVED: September 1990
CitadelP.O. i QR2Q
Sample f
4133343536373839
4180818283
NOTE: * denotes being checked.
** denotes checked.
Oz. Gold
0.002
IN ACCORDANCE WITH LONG-ESTABLISHED NORTH AMERICAN CUSTOM. UNLESS IT IS SPECIFICALLY STATED OTHERWISE COLD AND SILVER VALUES REPORTED ON THESE SHEETS HAVE NOT BEEN ADJUSTED TO COMPEN SATE FOR LOSSES AND GAINS INHERENT IN THE FIRE
ASSAY PROCESS.
BELL-WHITE ANALYTICAL LABORATORIES LTD.
Qkritfkat* ai: AnalgaiaFAX: (7O5) 672^5843 f
NO. 0?78
SAMPLE(S)OF: Fines (55)
DATE: September 27, 1990
RECEIVED: September 1900
SAMPLE(S) FROM:CitadelProject; P.O. #9829
Sample #
414041424344
Oz. Gold
Trace Trace Trace Trace Trace
RECEIVED Qry 2
Sample t Oz. Gold
NOTE: ** denotes checked.
IN ACCORDANCE WITH LONG-ESTABLISHED NORTH AMERICAN CUSTOM. UNLESS IT IS SPECIFICALLY STATED OTHERWISE COLD AND SILVER VALUES REPORTED ON THESE SHEETS HAVE NOT BECN ADJUSTED TO COMPEN SATE FOR LOSSES AND GAINS INHERENT IN THE FIRE
ASSAY PROCESS.
BELL-WHITE ANALYTICAL LABORATORIES LTD.
m
187, HAILEYBURY, ONTARIO)1KO
Qtarttftrai? ol0811
SAMPLE(S)OF: Rock
SAMPLE(S) FROM:Citadel Pro-ient: P.O. 9R29
DATE: October 4, 1990
RECEIVED: October 1990
Sample # Oz. Gold
4145 Trace
IN ACCORDANCE WITH LONG-ESTABLISHED NORTH AMERICAN CUSTOM. UNLESS IT IS SPECIFICALLY STATED OTHERWISE COLD AND SILVER VALUES REPORTED ON THESE SHEETS HAVE NOT BEEN ADJUSTED TO COMPEN SATE rpR LOSSES AND CAINS INHERENT IN THE FIRE
ASSAY PROCESS.
BELL-WHITE ANALYTICAL LABORATORIES LTD.
PI*
QI?rttfirate 0|f AttalgaiaNO. 0856
SAMPLE(S)OF: Hock (30)
SAMPLE(S) FROM: CitadelProject: P.O. 9829
DATE: October 16, 1990
RECEIVED: October 1990
RECEIVED OCT 2 2 1990
Sample #
4146474849
415051525354555657
Oz. Gold
0.008 0.002 0.002 0.012 0.004 0.004 0.004 0.002 Trace 0.006 0.010 0.006
** denotes checked.
IN ACCORDANCE WITH LONG-ESTABLISHED NORTH AMERICAN CUSTOM. UNLESS IT IS SPECIFICALLY STATED OTHERWISE GOLD AND SILVER VALUES REPORTED ON THESE SHEETS HAVE NOT BEEN ADJUSTED TO COMPEN SATE FOR LOSSES AND GAINS INHERENT IN THE FIRE
ASSAY PROCESS.
BELL-WHITE ANALYTICAL LABORATORIES LTD,
PCX
BELL -WHITE ANALYT CALP.O. BOX 187. POJ 1KO
HAILEYBUFlY, ONTARIO-S*3Mi'p;?rEL: ;'672-31O7 ;fe; .••:' "*- 672-5843
Ql^rtifirate ofNO. 0978
SAMPLE(S)OF: Rock (48)
Mr. R. Reid, Citadel
DATE: November 14, 1990
RECEIVED: November 1990
SAMPLE(S) FROM: Magpie R
Saiple iOz. Gold Au ppb Ag ppi Ho ppi Pb ppn in ppi l Co ppi
415t Trace 4159 Trace
IN ACCORDANCE WITH LONG-ESTABLISHED NORTH AMERICAN CUSTOM. UNLESS IT IS SPECIFICALLY STATED OTHERWISE GOLD AND SILVER VALUES REPORTED ON THESE SHEETS HAVE NOT BEEN ADJUSTED TO COMPEN SATE FOR LOSSES AND GAINS INHERENT IN THE FIRE
ASSAY PROCESS.
BELL-WHITE ANALYTICAL LABORATORIES LTD.
Ministry ofNorthern Developmentand Mines
Ontenos
/Tr(
MiniWActReport of Work(Geophysical, Geological and Geochemical Sui
4iNiSNEeeia 2 .13393 MCMURRAY
/fi1
900
Type 61 Survey(s) Mining Division Township
-frrfUX)Recorded Holder(s) Prospector's Licence No.
Telephone No.
Survey Company
2^1Name and Address of Author (of Goo-Technical Report)
- r h A** 13Name and A
•Z. 6 4'tfjgA*A~V*rrDate of Survey (from 6 tp)/9 /coyMf \\ Mo | Yr. j Day | Mo. |
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
- Other
Geological
Geochemical
Geophysical
- Electromagnetic
- Magnetometer
- Other
Geological
. Geochemical
.
Electromagnetic
Magnetometer
Other
Total miles flown over claim(s).
**)Uv 7 f To
DWr
'
&O
Days per Claim
TTTT
——— \
nc^irDays per
Claim
Recorded^Holder or Agerip(Skinature)
)E(
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Mining ClaimPrefix
5SM
1' ' H
13
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9Cj\
99;
Number
|?77sr*"77fC
37777177K
^779*7
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Mining ClaimPrefix
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NumberMining Claim
Prefix
|SUORMRM
MINING OJV. jm H C t \/ Ja-***-- U C 1 V
NUY 281891
'ilftlliKi \^\\
Ssf
IVEDM880 ——•"••^^
5 LAN! S SECT'ON
Number
C IJ||
M|fij6
3fi O't -
IEC~OEt^
j UlMIMft 1 A
1 ^0P
EiVEDt&m —MHO ccorinwnlliiinu W nw wi*viivii
Total number o1 mining claims covered by this report of work. f
Certification verifying Report of Work1 hereby certify that 1 have a personal and intimate knowledge of the facts set forth in this Report of Work, having performed the work or witnessed same during and/or after its completion and annexed report is true.Name And Address of Person Certifying
iPos Telephone No. r*) S/
^-For Office Use Only
Total Days Cr. Recorded
/Od
1362 (89(06)
Date RecordedDate Rec
, J 3,
foeDate Approved as Recorded
Mining
Provincial Manager, Mining Lands
ii^ffl/L ^A^iJU
Received StampSAULT STE. MARIE MINING DIVISION
RECEIVED
13 DEC 1990 PM
'ntario
Ministry ofNorthern Developmentand Mines
Ministere du DeVeloppement du Nord et des Mines
March 7, 1991
Mining Lands Section4th Floor, 159 Cedar StreetSudbury, OntarioP3E 6A5
Telephone: (705) 670-7264 Fax: (705) 670-7262
Your File: Our File:
W. 9005. 305 2. 13693
Mining RecorderMinistry of Northern Developmentand Mines875 Queen StreetP. O. Box 669SAULT STE MARIE, OntarioP6A 2B3
Dear Sir/Madame:
RE: Notice of Intent dated January 24, 1991 forGeological Survey submitted on Mining Claims SSM 937796 e t al in McMurray Township.
••^••••^.••^•••^•••••••-••^.•^•••W^CMVWVBBMVICIBMVM^BWVWMB.W.BWMMO.MBWMMWt-HWBWMWWWW
The assessment work credits, as listed with the above-mentioned Notice of Intent have been approved as of the above date.
Please inform the recorded holder of these mining claims and so indicate on your records.
Yours sincerely,
Ron. C. Gas hi ns lProvincial Manager, Mining LandsMines & Minerals Division
LJ/jl Encl:
cc: Mr. W. D. TiernanMining and Lands CommissionerToronto, Ontario
Citadel Gold Mines Inc. Wawa, Ontario
R. G. Reid Wawa, Ontario
Ministry ofNorthern Developmentand Mines
Technical Assessment Work Credits
Ontario Dcte
Jan. 24/91
Pile
?. 13693Mlnlna ReeorcUrt *teporWoffe?005.305
t of
Accorded Holder
Citadel Gold Mines In?.Township or Area
lMrMurray Tnwnc.Mn
Type of survey and number of Assessment days credit per claim
Geophysical E"*e*'Afr"*g"**ie dayt
U.gn.tnr^t.r d*Vt
Radiometric ,... ,... - days
Induced poteriratlon . .. ,... . days
nth*r davs
Section 77 (19) See "Mining Claims Assessed" column
f*wl"g'fltl 20 (taut
finnchAinlnil davs
Man days Q Airborne D
Special provision Q Ground Q
I~L Credits have been reduced because of partial coverage of claims.
Q Credits have been reduced because of corrections to work dates and figures of applicant
Special credit* under section 77 (16) for the following i
Mining Claims Aeietsed
SSM 937796 -799 Incl.
.
nlnlng daJms
10 days geology on SSM 937795l
No credits have been allowed for the following mining dalmsQ not sufficiently covered by the survey Q Insufficient technical data filed
The Mining Recorder may reduce the above credits If necessary in order that the total number of approved assessment day* recorded on each claim does not exceed the maximum allowed as follows: Geophysical - 80; Geoloflocal - 40; Geochemical - 40; Section 77(19) *00.
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