on mine centre project of the hanna mining company€¦ · in 1911, a. c. lawson (1918) and in 1934...

S2C16SW0428 2 .2297 L ITTLE TURTLE LAKE 010

MAGNETIC REPORT

on

MINE CENTRE PROJECT

of

THE HANNA MINING COMPANY

by

John F. Muhic

February 9, 1976

THE HANNA MINING COMPANY MINE CENTRE FKDFERTY

LIST OF CIAIMg

A . Unpateflted clgijns Jhflld by The Hanna Mining Company.

K-419522-531 - 10

K-413966-972 - 7

K-414984-415000- 17

K-419501-03 - 3

K-419505-52l - 17

K-412629-662 - 34

K-434751-739 - 39

K-434791-795 - 5

K-434797-805 * 9

K-412716-723 - 8

Total -149

B. Patented cljalrns optioned from G t L. Pidgeon of Wabigoon* Ontario

K, 298

K. 300

K. 301

P. 683

K. 304

Total

- 1

* 1

- 1

- 1

- 1

- 5

MINE CENTRE

INTRODUCTION

The Hanna Mining Co. was originally attracted to the area by zinc showings on patented claims P. 683 and K. 301. A total of 149 claims were staked and 5 patented claims were optioned by The Hanna Mining Company*

The property was covered by a grid of picket lines at 400-foot intervals. During 1975, a geological survey, two types of electromagnetic surveys, and a magnetometer survey were conducted on the claim block.

The project was supervised by H* Willson, B. Se, and assisted by A. Little, 8. Se, J. Muhic, B. Se, R. Tanaka and J. Spiteri under the direction of Nelson Hogg, District Geologist for The Hanna Mining Co. After September l, John Muhic supervised all field work on the project) and the plotting and interpretation of data.

LOCATION ft ACCESS

The property crosses Ontario Hwy.ll about Sfc miles east of Mine Centre. It extends 3 miles southwest of the highway, and to the east it occupies the ground between Hwy.ll and the Little Turtle River for a distance of 4 miles.

The west end can be reached by old logging roads branching east from the Shoal Lake Rd. The eastern portion is reached from Hwy.ll, from the road to Bowes Camp, and from the CNR which traverses the central part of the claims.

Three power lines, Highway 11, and the CNR cross the property in an east-vest direction.

In 1969, Kerr Addison Mines Ltd. conducted a geophysical and geological survey over the area of the property south of Hwy.ll. The geophysical survey was done using a Crone JEM instrument. The JEM survey did not detect any anomalies. As far as it is known no geophysical survey was carried out on the rest of the property.

The area, however, has been heavily prospected for gold dating back to 1893. Abundant trenches and occasional shafts scattered throughout the property serve as evidence of the prospecting activity*

frINE CUTTING

Because of a bend in the geologic structure, two grids of picket lines were cut. A base line bearing N550E was cut from 60+OOE to 200+OOE and a base line bearing 90O Astronomic was cut from 198+OOE to 400*OOEast. All base lines were transit controlled. Tie* lines were cut at 20+OON, 20400S, 40+OON and 40+OOS, but were not transit controlled. Picket lines were cut perpendicular to the base lines at 400-foot intervals* Some lines across bad swamps and ponds were completed after freeze-up*

MINE CENTRE Page 2

The line-cutting was done under contract. Work was begun under Mr. C. D. Huston o i' Winnipeg and completed under the super vision of Mr. Scott Waldie, Red Lake, Ontario.

A total of 6.5 miles of base lines, 11.07 miles oi tie lines and 106.94 miles of picket lines were cut. Because of reconnaisance mapping, the decision was made to do no further work on 29 claims in the gouthwest end of the property. The grid and the surveys cover 120 unpatented claims and 5 patented claims. All geological surveys and geophysical surveys were carried out using the same grid.

PERSONNEL

The magnetometer survey was conducted by Joseph Spiteri and John Muhic during the summer and fall of 1975. The results ore plotted arid contoured on 8 standard sized sheets of 36" X 44".

GENERAL GEOLOGY

Even though there was an abundance of prospecting activity on the property, little geological mapping has been carried out by Ontario Dept. of Mines or the G.8.C. In 1911, A. C. Lawson (1918) and in 1934 T. L. Tanton (1935,1936) mapped the Mine Centre area including the west end of the Hanna property. To the east of the property, the Bennett-Tanner area was mapped by W. L. Young (1960) in 1958.

The property is in general underlain by felsic to rhyolitic volcanics interbedded with intermediate volcanics and intruded by quartz gabbro. It is bounded on the north by highly sheared, carbona- tized and chloritized intermediate volcanics which lie just south of the Quetico Fault. The southern boundary consists of the Seine River group of conglomerates and intermediate volcanics. To the weet, the volcanics pinch out into the Seine conglomerate.

There is one elliptical mass of mafic volcanics extending from L312E to L340E north of Tie Line 20+OON. The intermediate volcanics occur in bands up to 300 ft. wide interbedded with felsic volcanics, and in greater widths to the north and south of the felsic volcanics*

Most of the property is underlain by felsic volcanic rocks which include uniform, fine grained, sericitized rhyolite with well de veloped quartz eyes.

The quartz gabbro occurs as two massive sill like sheets that appear to be conformable with the surrounding volcanics. The gabbro is characterized by a high magnetic relief.

A general geology map at a scale of l inch equals ^ mile is bound into the report.

INSTRUMENT

The survey was conducted using a Scintrex MF-2 Fluxgate mag netometer with a sensitivity of 20 gammas per scale division on the most sensitive scale.

MINE CENTRE Page 8

MCTHOp OF SURVEY

Base stations were established along the base lines and tie lines of the grid at 100 foot intervals. This was done by reading the base stations a few at a time, checking back constantly to an already established base station and then carrying the survey ahead. On this property a total of 367 base stations were established over 16.52 miles of the lines and base lines.

The picket line grid was then run in closed loops, checking in at the base stations on the base line or tie line at regular periods. The readings were taken at 50-foot intervals except in anomalous areas where 25-foot readings were taken. A total of 11,685 readings were taken over 104.87 wiles of picket line*

RESULTS fr CONCLUSIONS

The readings were plotted on eight 36" X 44" sheets and contoured* Copies of the maps are enclosed with the report*

The contour pattern shows a strong trend sub parallel to the base lines. Geological units can be successfully traced under over* burden and thus the magnetometer readings were useful in geological interpretation. The moat striking magnetic relief is associated with the two gabbroic sills* One extends from the eastern boundary and pinches out at L212+OOE. A second sill occurs south of the base lines between L252+OOE and line 300+OOEast.

4

There are scattered one-station anomalies throughout the property that do not extend to adjacent picket lines. One example of this is on L164E 10+008. These small magnetic anomalies ire probably due to very narrow magnetic bands that have been observed in a few places on the property. They occur in the felsic and intermediate volcanic units*

It is interesting to note that the intermediate volcanic! along the northern boundary of the claim group have very low magnetic properties. In contrast the intermediate volcanics along the southern boundary between L60+OOE and 228+OOE, have relatively high magnetic relief.

REFERENCES

Lawson, A. C. - The Archean Geology of Rainy Lake Re - Studied G. S. C. Menu 40 ~ map no.98a-1913.

Lawson, A. C. -"Report on the Geology of the Rainy Lake Region" Annual Report, G. S. C .Vol. Ill, 1888 Report F.

Tanton, T*L* ~ Geological Survey of Canada Map 334A Mine Centre Area * 1936. l in.* fc mile.

Tanton, T.L. -Preliminary Report on Mine Centre Area, Ontario, G. 8. C*, Jan. 1935.

Young, W. L. -Geology of the Bennett-Tanner area, Ont, Dept. of Mines Vol.IXlX Pt 4, 1960.

February 9,1976 John F. Muhic,B.8c•.***.....**********(**

S2C16SW0428 2.2297 LITTLE TURTLE LAKE 020

MINE CENTRE PROJECT


ELECTROMAGNETIC REPORT

on a

CRONE C.E,M. SURVEY

by

JOHN F. HUIIIC, B.Se.

FEBRlttRY 9 t 1976

THE HANNA MINING COMPANY MINE CENTRE PROPERTY

LIST OF CIAIHS

A. Unpatented c^|^fiJi/eld Jby Tl\(B Hfflng M*ft*.!\fl Company*

K-419522-S31 - 10

K-413966-972 - 7

K-414984~415000- 17

K-419501-03 - 3

K-41950S-521 - 17

K-412629-662 - 34

K-434751-789 - 39

K-434791-795 - 5

K-^34797-805 - 9

K-412716-723 - 8

Total -149

B. Patented claims optioned froro G* L. Pidceon ol Wabigoon* Ontario

K, 298

K. 300

K. 301

P.683

K. 304

Total

- 1

- 1

- 1

- 1

- 1

- 5

P^ECTROMAGNETIC IMPORT GEM SURVEY

INTRODUCTION

The Hanna Mining Co. was originally attracted to the area by zinc showings on patented claims P.683 and K.301. A total of 149 claims were staked and 5 patented claims were optioned by The Hanna Mining Company*

The property was covered by a grid of picket lines at 400-foot intervals. During 1975, a geological survey, two types of electromagnetic surveys, and a magnetometer survey were conducted on the claim block*

The project was supervised by H. Willson, B.Se, and assisted by A. Little, B .Se, j. Muhic, B.Se, R, Tanaka and J* Spiteri under the direction of Nelson Hogg, District Geologist for The Hanna Mining Co* After September l, John Muhic supervised all field work on the project, and the plotting and interpretation of data.

LOCATION 6 ACCESS

The property crosses Ontario Hwy.ll about 3fc miles east of Mine Centre* It extends 3 miles southwest of the highway, and to the east it occupies the ground between Hwy.ll and the Little Turtle River for a distance of 4 miles.

^

The west end can be reached by old logging roads branching east from the Shoal Lake Kd. The eastern portion is reached from Hwy.ll, from the road to Bowes Camp, and from the CNR which traverses the central part of the claims.

Three power lines, Highway 11, and the CNR cross the property in an east-west direction.

FORMER WORK

In 1969, Kerr Addison Minos Ltd. conducted A geophysical And geological survey over the area of the property south of Hwy.ll. The geophysical survey was done using a Crone JEM instrument. The JEM survey did not detect any anoiualiee. As far as it is known no geophysical survey was carried out on the rest of the property.

The area, however, has been heavily prospected for gold dating back to 1893. Abundant trenches one! occasional shafts scattered throughout the property serve as evidence of the prospecting activity*

CUTINGBecause of a bend in the geologic structure, two grids of

picket lines were cut. A base line bearing NSS^ was cut from 60+OOE to 200+OOE and a base line bearing 900 Astronomic was cut from 198+OOE to 400+OOEast. All base lines were transit controlled. Tie-lines were cut at 20+OON, 20+008, 40+OON and 40+OOS, but were not transit controlled* Picket lines were cut perpendicular to the base lines at 400-foot ^intervals. Some lines across bad swamps and ponds were completed after freeze-up.

'RE " OEM Sl. Pae 2

The line-cutting was done under contract t Work was begun under Mr. C. D* Hutton of Winnipeg and completed under the super* vision of Mr, Scott Waldie, Reel lake, Ontario.

A total of 6.5 miles of base lines, 11.0? miles of tie lines and 106.94 miles of picket linoe were cut. Because of reconnaisance mapping, the decision was made to do no further work on 29 claims in the southwest end of the property. The grifl an,^ foe surveys cover

j.20 unpa tented claims and 5 pat entetV claims. All geological surveys end geophysical surveys were carried out using the same grid,

The Crone C. E. M. Survey was conducted by Joseph Spiteri, Rod Tanaka and John Muhic during the sunnier and fall of 1975. The results were plotted and profiled on 8 standard 36" X 44" sheets.

GENERAL CEOLQGY

Evon though there wr.s an abundance of prospecting activity on the property, Llttl.o geological mapping has been carried out bv Ontario Dept, of Hineo or the G.S.C. In 1911, A. C. lawson (1913) and in 1954 T. L* Tanton (1935, 1936) rapped the Mine Centre area including the west end of the Hanna property, To the east of the property, the Bennett-Tanr.or area was iwppecl by W, t. Young (1960) in 1968,

The property is in general underlain by felsic to rhyolitic volcanics interbedded with intermediate volcanics and intruded by quartz gabbro. It is bcrmded on the north by highly sheared, carbona- tized and chloritized intermediate volcanics which He just south of the Quetico Fault. The southern boundary consists of the Seine River group of conglomerates arid intermediate volcanics. To the west, the volcanics pinch out into tho Seine conglomerate.

There is one elliptical mass of mafic volcanics extending from L312E to L340E north of Tio Line 20+OON, The intermediate volcanics occur in bands up to 800 ft. wide interbedded with felsic volcanics, and in greater widths to the north and south of the felsic volcanics,

Most of the property is underlain by felsic volcanic rocks which include uniform, fine grained, rericitized rhyolite with wall df* veloped quartz eyes.

The quartz gabbro occurs as two massive sill like sheet* that appear to be conformable with the surrounding volcanics. The gabbro la characterized by o high magnetic relief.

A general geology map at a scale of l inch equals \ mile is bound into the report.

INSTRUMENT

The survey was conducted using a Crone C.E.M. unit, It con sists of two identical coils that can alternately transmit and receive. The operating range of the coils is up to 200 meters. Measurements are Biade by visual null on the field strength meter and by audio null through crystal earphones* The inclinometer has a range of 200 degrees and an accuracy of * 0.5 degrees. The instrument has three frequencies 5010 H*, 1830 Hz and 390 Hz.

MINE CENTRE - GEM SURVEY Page 8

METHOD O

The Horizontal Shootbeck EM method was employed during this survey. With this method, both operators traverse along the same picket line. Both, in turn, transmit and receive, measuring the dip angle of the iield. The two angles are then added together and equal "O" li no conductor is present* The result is plotted at the mid-point between the two coils. One advantage of this system is that no cor* rections ere necessary because of topography.

A 300-foot coil spacing was used during the survey* Readings were taken at 100-foot intervals except in anomalous cones, where readings were taken at 50-foot intervals. The basic coverage was con ducted using the medium frequency of 1830 Hz. Where anomalous tones were encountered, both 1830 and 390 Hz were recorded.

A total of 108.36 miles of picket line were covered* volved 6264 readings at 1830 Hz and 2009 readings at 390 Hs.

RESULTS l CONCLUSIONS

This in-

The readings were plotted on eight 36" X 44" sheets and profiled* Copies of the maps are enclosed with the report*

As a result of the two high voltage power lines, one low voltage power line (along Hwy 11) and the railway, severe electromagnetic inter ference was encountered in their vicinity. Thus any anomalous readings obtained 800 to 900 feet on either side of the high voltage lines or 400 to SOO feet on either side of the railway and the highway can be attribu ted to the electrical interference* Anomalies found on the rest of the property along with their interpretation are summarized in the following table. The interpretations are based on consultations with Duncan Crone who designed the instrument.

Station Interpretation.. Surface Geology

L100E

(based on consultation with D.Crone)

8+508 Good conductor Depth 50-75' Width 50' Dip 450S

Felsic Volcanics

L104E 12+003 Bedrock conductor. Steep dip tosouth. Depth- 75 feet

Spruce muskeg

L112E 12+508 Deep narrow bedrock conductor.Depth- over 100 feet*

Spruce muskeg

L128E 10+OOS Good conductor dipping south 50 Muskegto 75' deep

L132E 16+008 Narrow deep conductor Muskeg

CETRE - GEM SURVEY

U40E 11*008 Good narrow, very deep (150 ft)conductor

Pace 4

Muskeg

L200E 2S+OON Weak multiple conductor about SO' deep

Sand plain

L204E 19+40N- Harrow, banded, multiple conductor. Sand plain 21+OON

L208E 14+50N Narrow, multiple conductor Sand plain

L224E 37+7ON- Anomalous readings only in medium 42+40N (1830Hz) frequency indicate prob

ability of highly conductive overburden.

Spruce swamp

L228E 40+50N Good target* Poor conductor. Steep Spruce swamp dip to north. Depth 50-75'.

L232E 87-HJON- Only medium frequency anomalous 44+OON readings- probably overburden.

Spruce swamp

L236E 15+50N Good conductor. Narrow. Bteep dip Sand plain to north. Depth SCK75 1

t236E 38+50N*- Probably conductive, overburden. 44+OON Possibly poor bedrock conductor,

at S9+SON.

Spruce swamp

L240E S8-K)ON Deep good conductor Spruce

L240E 42-K)ON Deep good conductor Spruce swamp

L240E 8-K)ON Parallel, multiple weak conductors. Sand plain

L240E 16+20N Parallel, multiple weak conductors. Sand plain

L240E 17+OON parallel, multiple weak conductors. Sand plain

L244E 44+OON Conductive overburden. Spruce swamp

MIKE CENTRE * OEM SURVEY Page S

iiag~L244E

L256E

L264E

L264E

L272E

L296E

L304E

W12E

L316E

L360E

L380E

L384E

Ration

19+50N

13+20N

20+OON

23+OON

23+OON

2+808

6+008

37+80N

4+OOS

18+50N

10+OON- 12+60N

28+OON

u jLi^^rpretsitip^ , {Surface Geolofiv

Deep, poor conductor, steep dip north*

Weak, multiple conductors, deep.

Weak, multiple conductors

Weak, multiple conductors

Weak, multiple conductors*

Weak, narrow bedrock conductor

Weak, poor conductor, high mag netics due to gabbro.

Deep conductor, vertical dip.

Narrow, weak, near surface conductors*

Narrow, multiple, weak conductors.

Shallow, poor, multiple conductors*

Good conductor near surface

Sand Plain

Rhyolite

Felsic volcanic

Rhyolite

Rhyolite

Tag alder swamp

Quarts gabbro

Intermediate Tuff

Sand ft Boulders

Marsh

Sheared Quarts Gabbro

Interbedded Inter** mediate f, Felsic Volcanics*

It should be noted that none of the above anomalies} with the exception of that on L304 and 6+OOS, have coincident magnetometer anomalies* Also, the conductors have a very short strike length. The majority are found on only one line and no conductor crosses more than two adjacent picket lines.

Another electromagnetic survey using the APEX Max Min 11 system run over the best Crone C.E.M* conductors failed to confirm any of them* As a result, a decision was made to drill only the best three C.E.M. anomalies on the property. The anomalies drilled were (1) L100E 8+508* (2) L236E 1S+SON and L228E 40+50N.

The first hole intersected several cones of seamy and-disseminated pyrite with up to 153* sulphides. When the cross section of the diamond drill hole was drawn, the correlation between any of the sulphide sonea and the surface C.E.M. anomaly was dubious at best.

MIE E - GEM SURVEY e 6

The second hole on line 236E intersected a 2.5 foot Bone of 5^ sulphides tlvat appeared to correlate with the C. E. M t anomaly, but it is doubtful that the sulphide content is high enough to be detected by the instrument.

The third hole on line 228E encountered no bedrock conductor, but the overburden was 193 feet doep ond consisted of sand and red clay. Because of the depth and nature of the overburden, the writer concludes that the anomaly was caused by it*

A separate detailed report on the diamond drilling program has been submitted to the government*

Lawson, A .C. - The Archean Geology of Rainy Lake Re ~ Studied G. S. C. Mem. 40 * nap no.98a~1913.

Lawson, A. C.- "Report on the Geology of the Rainy Lake Region*1 Annual Report, G. 8. C. Vol.111, 1888 Report F.

Tanton, T .L. - Geological Survey of Canada Map 334A Mine Centre Area - 1936. l in. B fc mile*

Tanton, T.L. - Preliminary Report on Mine Centre Area, Ontario,G. S. C., Jan. 1935.

^ Young, W. I.*- Geology of the Bennett-Tenner area,

Ont. Dept. of Mines Vol.IXUC Pt 4, 1960

*...l..**..***.February 9, 1976 JohnNfc. Muhic, B.80

52C16SW8428 2 .2297 L ITTLE TURTLE LAKE 030

MINE CENTRE PROJECT


ELECTROMAGNETIC REPORT

on an

APEX SURVEY

by

JOHN F. MUHIC

February 10, 1976

THE HANW MIKING OOMBUN NINE CENTRE PROPERTY

LIST OF QAIMS

A*

K-419522-531 - 10

K-413966-972 - 7

K-4M984-416000- 17

K-419501-08 * 3

K-419505-521 - 17

K-412629-662 - 34

K-434751-789 - 39

K-434791-795 - S

K-434797-805 * 9

K-412716*723 - 8

Total

K.298

K* 300

K. 301

P.688

K. 304

Total

- 1

- 1

- 1

* 1

- 1*"""5

MINE CENTRE ELECTROMAGNETIC REPORT

APEX SURVEY_____

INTRpDUCTIpN

The Hanna Mining Co. was originally attracted to the area by zinc showings on patented claims P.683 and K.301. A total of 149 claims were staked and 5 patented claims were optioned by The Hanna Mining Company,

The property was covered by a grid of picket lines at 400-foot intervals t During 1975, a geological survey, two types of electromagnetic surveys, and a magnetometer survey were conducted on the claim block.

The project was supervised by H. Willson, B.Se, and assisted by A. Little, B.Se, J. Muhic, B.Se, R, Tanaka and J. Spiteri under the direction of Nelson Hogg, District Geologist for The Hanna Mining Co* After September l, John Mollic supervised all field work on the project, and the plotting and interpretation of data.

The electrical interference from tha power lines and railway crossing the property invalidated the readings of the Crone GEM in their vicinity. Therefore, a decision was cade to survey these areas as well as some of the better GEM conductors with an APEX Parametric! Max Min 11 system.

LOCATION 6 ACCESS

The property crosses Ontario Hwy.ll about Sfc miles east of Mine Centre* It extends 3 miles southwest of the highway, and to the east it occupies the ground between Hwy.ll and the Little Turtle River for a distance of 4 miles.

The west end can be reached by old logging roads branching east from the Shoal Lake Rd. The eastern portion is reached from Hwy.ll, from the road to Bowes Camp, and from the CNR which traverses the central part of the claims.

Three power lines, Highway 11, and the CNR cross the property in an east-vest direction.

FQRMERJJORK

In 1969, Kerr Addison Mines Ltd. conducted a geophysical and geological survey over the area of the property south of Hwy.ll. The geophysical survey was done using a Crone JEM instrument. The JEM survey did not detect any anomalies. As far as it is known no geophysical survey was carried out on the rest of the property.

The area, however, has been heavily prospected for gold dating back to 1893. Abundant trenches and occasional shafts scattered throughout the property serve as evidence of the prospecting activity*

MINE CEflTfiE, Eagq 2

LINE CUTTING

Because of a bend in the geologic structure) two grids of picket lines were cut. A base line bearing N5S0E was cut from 60+OOE to 200+OOE and a base line bearing 900 Astronomic was cut from 198+OOE to 400+OOEast. All base lines were transit controlled) Tie-lines were cut at 20+OON, 20+008, 40 -K) ON and 40+OQS, but were not transit controlled. Picket lines were cut perpendicular to the base lines at 400-foot in tervals* Some lines across bad swamps and ponds were completed after freeze-up.

The line-cutting was done under contract* Work was begun under Mr* C* D* Huston of Winnipeg and completed under the supervision oi Mr* Scott Waldie, Red Lake, Ontario.

PERSONNEL

The Apex hex Hiri 11 survey was conducted under contract by Geosoarch Consultants Ltd., 100 University A ve., Suite 1114, Toronto, Ontario between September 16 and September 28, 1976, and between November 26 cud December S, 1975*

GEOLOGY

Even though there was an abundance of prospecting activity on the property, little geological mapping has been carried out by Ontario Dept. of Mines or the G. S. C. In 1911, A. C* Lawson (1918) and in 1934 T* L* Tanton (1985,1936) wapped the Mine Centre area including the west end of the Hanna property. To the east of the property) the Bennett-Tanner area was napped by W. L. Young (1960) in 1958*

The property is in general underlain by felsic to rhyolittc volcanics interbedded with intermediate volcanics and intruded by quartz; gabbro* It is bounded on the north by highly sheared) carbona- tized and chloritized intermediate volcanics which lie just south of the Quetico Fault* The southern boundary consists of the Seine River group of conglomerates and intermediate volcanics* To the west) the volcanics pinch out into the Seine conglomerate*

There 16 one elliptical mass of mafic volcanics extending front LS12E to LS40E north of Tie Line 20+OON. The intermediate volcanics occur in bands up to 800 ft* wide interbedded with felsic volcanics j and in greater widths to the north and south of the felsic volcanics.

Most of the property is underlain by felsic volcanic rocks which include uniform, fine grained, sericitlzed rhyolite with wall de veloped quartz eyes*

The quartz gabbro occurs as two massive sill like sheets that appear to be conformable with the surrounding volcanics* The gabbro is characterized by a high magnetic relief.

A general geology map at a scale of l inch equals ^ mile is bound into the report.

CEHTR

The survey was conducted using the new APEX Parametrics Max-Min 11 system. The unit was used on a horizontal loop mode which can be used with a coil separation up to 600 feet. It features automatic, direct readout of the In-phase and Quadrature components of the secondary field on S'g" size meters with a *fa to jjKMS reading repeatability. Operating frequencies include 222, 444, 888, and 1777 HK with a 0.2 Hz norncl receiver bandwidth. The system is reputed to be able to take valid readings underneath power lines. A built-in intercom system permits easy communication at any coil separation*

OF

The APEX system was used in a horizontal loop mode. Both operators traverse along the same picket line. When a station is reached, the transmitter is turned on and the receiver operator notes the In-phase and quadrature readings. The readings are plotted at the mid point between the two coils* Topographic effects are eliminated by tilting both tlie transmitter and receiver colls to maintain a ooplanar configuration . Doth coils have a built-in tilt-meter to co-ordinate tht angle of tilt for both operators.

During the survey a 400 foot coil separation was used and readings were taken at 100 foot intervals. A frequency of 888 He was used on this property except where some experimental work was done using different frequencies and coil separations 4

A total of 2,968 readings were taken over 61.89 miles of picket line*

OONCLUSINS

The readings were plotted and profiled on eight 86" X 44" sheets* Copies of the maps are included with the report.

No anomalies were detected by this survey* Moreover, when the Apex instrument was run over ground with GEM anomalies, it failed to confirm them. Directly under power lines, low anomalous readings are obtained, but meaningful readings are obtained until one coil is directly under the power line, so very little ground is eliminated from the survey*

The survey was very useful in helping to decide on a drilling program.

.•.*.*i... .jf ...t***...******************John rHluhic, B.Se

February 10, 1976 Geologist

MjNE ffiffftfi Page 4

REFERENCES

Lawson, A,C. * The Archean Geology of Rainy Lake Re - Studied G.3.C. Mem.40 - tap no.98a-1913.

Lawson, A,C. -"Report on the Geology of the Rainy Lake Region" Annual Report, G.S.C. Vol.111, 1888 Report F.

Tanton, T,L. - Geological Survey of Canada Map 384A Mine Centre Area - 1936. l in. s fc mile,

Tanton, T.t. - Preliminary Report on Mine Centre Area, Ontario, G.S.C., Jan.1935.

Young, W.L. -Geology of the Benriett-Tanner area, Ont. Depl. of Mines Vol.LXlX Pt 4, 1960

CERTIFICATE

I, John F. Muhic, of the city of Toronto, in the Province

of Ontario, hereby certify that:

1. I am a graduate in geology with the degree of B. Se. from the University of Toronto, 19751

2. That I am a full-time employee of The Hanna Mining Company, Room 805, 69 Yonge Street, Toronto, Ontario.

S* That the accompanying report is based on my personal knowledge of work done on the property, sup plemented by information from published governmentreports.

4. That I have no direct or indirect interest in the property.

JLjin F. Muhic,

Geologist

February 9, 1976

S2C16SW0428 2.2297 LITTLE TURTLE LAKE 040

GEOLOGICAL REPORT

on

MINE CENTRE PROJECT

of


by

Nelson Hogg

December 31, 1975

HINE CENTRE

INTRODUCTION}

The Hanna Mining Company was attracted to the Mine Centre area by G* L. Pidgeon of Wabigoon, who had exposed zinc mineraliza tion on two patented claims, F.683 and K.SOI. Pidgeon's five patented claims were optioned, and an additional 54 claims were staked in January, 1975. As work on these claims progressed, it became apparent that the favourable felsic rocks pinched out to the west but widened to the east, so 95 additional claims were staked during the summer of 1975 to cover the geologically attractive area. The property has a length of 1\ miles and tt maximum width of 2 miles*

The entire property was covered by a grid of picket lines at intervals of 400 feet, and the grid was used to carry out a geological survey, two types of electromagnetic surveys, and a magnetometer survey during 1975.

The project was supervised by H* Willson, BA.Sc. assisted by A* Little, B Se., J. Muhic, B Se., R. Tanaka and J. Spiteri, under the direction of Nelson Hogg, District Geologist for The Hanna Mining Company.

Application was made under the Ontario Mineral Exploration Assistance plan to obtain assistance in the amount of one-third of expenditures on the property up to a maximum #100,000.

LOCATION fr ACCESS*

The property crosses Ontario Highway No.11 about Sfc miles east of Mine Centre, or 43 miles east of Fort Frances. It extends 8 miles south-west of the highway, almost to Shoal take, and to the east it occupies the ground lying between Highway 11 and the Little Turtle River for a distance of 4 miles t

The west end la reached by old logging roads branching east from the Shoal Lake Roed. The eastern portion is reached from Highway 11, from the road to Bowes Camp, and from the CNR, which traverses the central part of the claims.

Three power lines, Highway 11, and the C.N. Railway cross the property in an east-west direction.

ffiSTORY OF THE MINE CENTRE AREA?

Prospecting for gold in the Mine Centre area dates back to 1893 when prospectors entered the area from Minnesota * Quite a number of patented claims that ere still in good standing were patented before 1900. in 1934, T. L* Tanton l** mapped the area for the Geo logical Survey of Canada, and at that time he reported the existence of more than 60 gold-bearing veins in the quartz porphyry mass south-east of Bad Vennillion Lake, plus at least 20 gold-bearing veins in the quartz porphyry lying close to the north shore of the same lake*

MIKE CETRE

The titaniferous magnetite deposits west of Bad Vermilllon Lake were also investigated by?prospectors in the early 1900's and are described by A. C. Lawson in 1918. In 1957 some of these occur rences were drilled by Stratraat Ltd.

Copper has also been found in the gabbro and volcanic rocks of the area. In 1916 the Port Arthur Copper Company worked on a copper deposit located 3 miles west of Mine Centre, on claim HP 187. Another copper occurrence in gabbro was developed by International Copper Company on clnlro IT 388 located l mile south-east of Mine Centre.

LINE-CUTTING l

Because the geological structure bends, two grids of picket lines were cut. A base line bearing N550 Hast was cut from 60+00 East to 200+00 East, and picket lines were cut at 400-foot intervals to the property boundaries. The baseline was not cut from 0+00 to 60+00 East because the decision was made to drop 29 claims forning the south-west corner.

At 198+00 East, a second base line was started, bearing 900 Astronomic. This base line was extended to the west for 800 feet, and to the east from 198+OOEast to 400+00 East. All base lines were transit-controlled. Tie-lines were cut at 20+00 North, 20+00 South, 40+00 North and 40+00 South, but they were not transit-controlled, to they do not maintain a fixed distance from the base line* Picket lines were cut at 400-foot intervals from the base line to the property boundaries except in places where ponds or swamps prevented cutting* In these cases the lines were cut back from a tie line toward the base line. Some lines across bad swamps and ponds were completed in November after freeze-up.

The following table sunnarizes the line-cutting operation*

___________________Miles^^^^^ Base Lines 6.5 ,;

Tie Lines 11,07

Picket Lines 106.94 ^^f (..' ^ -" '

All picket lines were cut under contract* Work was started by Mr. C. D. Huston of Red Lake and Winnipeg, and was comploted by Mr. Scott Waldie of Red lake. Attempts to use local labour were largely unsuccessful, although the local unemployment rate is high* Progress was slow due to Inability of the contractors to attract labour, and in the end nearly all the line-cutters were imported from other parts of the province.

Names end addresses of the contractors are listed belowt

Mr. C. D. Huston94 Columbus Crescent,Westwood, Manitoba.

Mr. J. Scott Waldie, Box 52, Madsen, Ontario.

MIflfi CENTRE Page 8

OWNERSHIP*

The 149 ompatented claims are held by The Hanna Mining Company, Room 80S, 69 Yonge Street, Toronto. These claims are numbered as follows:

K-419522-531 - 10

K-413966-972 - 7

K-414984-41SOOO- 17

K-419501-03 - 3

K-419505-521 - 17

K-412629-662 - 34

K-434751-789 - 39

K-434791-795 - S

K-434797-805 - 9

K-412716-723 - 8

Total -149

Five patented claims, K298, K300, K301, P683 and K804 are held under an option agreement with G. L. Pidgeon of Wabigoon, Ontario*

The Hanna Mining Company is responsible tor submitting assessment work on the unpatented claims i

One unpatented claim (K-416612), and one patented claim (KS88) located within the Hanna claim block, are not owned by The Hanna Mining Company*

GEOLOGICAL MAPPING;

Reconnaissance mapping along the claim boundaries of the original 54 claims was started on May 11, 1976 and mapping continued until October. Ae a result of the early reconnaissance mapping, the decision was made to do no work on the 29 claims forming the southwest end of the property, but to stake additional claims at the northeast end* Eventually a total of 149 claims were staked, but work was confined to 120 unpatented claims and 5 patented claims. These claims were mapped on picket lines 400 feet apart at a scale of l inch equals 200 feet* Mapping was done on 107 miles of picket line, 6^ miles of base line, and 11 miles of tie line.

Mr. Hugh Willson was in charge of the mapping and was assis ted at different times by A. Little, J. Spiteri, R. Tanaka, and J.Muhic.

Results are plotted on 8 standard-sized sheets of 36" X 44".

MINE CENTRE

REGIONAL GEOLOGY?

Although the Mine Centre district has been a focal point for prospecting since 1880, little detailed geological mapping has been carried out by the Ontario,. Department of Mines or the Geological Survey of Canada. A. C. Lawson mapped the area in 1911, and started the long-stending discussion about the age relationship between the Seine Series, the Keewatin Series, and the Couchiching Series of sedimentary rocket

T. L. Tanton ^*2 made a more detailed map of the Mine Centre gold camp in 1934, mapping at a scale of l inch equals 1/2 mile.

Both Lawson and Tanton mapped to a north-south line about 3 miles east of Mine Centre. Ho detailed mapping has been done to the cast of this line for 8 miles, which marks the west boundary of the Bennett-Tanner area, mapped in 1958 by W. L. Young 3 for the Ontario Department of Mines. Most of the property held by The Hanna Mining Company is in this 8-mile gap of unmapped ground. Neither Tanton 1 s Mine Centre map, nor Young's Bennett-Tanner map designate a unit of felsic volcanic rock, which is the principal rock-type on the Hanna claims t Tanton grouped all the Keewatin volcanic rocks together as greenstone, and Young apparently mapped the felsic volcanics as part of a "chloritic schist and tuff" unit. Later compilations 4'5 by the Ontario Department of Mines do not resolve the problem, so a modified table of formations for the area is used in this report*

Only the geology to the south of the Quetico fault if consi dered, The Quetico fault zone follows the Little Turtle River, and the Hanna property lies to the south of the fault. The Quetico fault i* one of the major old faults of the Canadian Shield, ranking in importance with the Porcupine-Destor fault and the Kirkland-Malartic fault. It can be traced from the lake of the Woods to Lake Superior, a distance of more than 200 miles, and it IB characterized by a profound change in lithology of the Archean rocks on the two sides of the fault*

A table of formations for rocks in the Mine Centre area, south of the Quetico fault is given below:

rchean t

l

Sjeine - Felsic Intrusive Rocks - Granite, Quartz Porphyry* - Basic to Ultrabasic Intrusive Rocks - Anorthositic

Gabbro, Gabbro, and Peridotite* -Intrusive Contact

Seine - Conglomerate, graywacke.

Keewatin -Intermediate, Basic and Felsic Volcanic Rocks.

Couchiching- Graywacke, argillite and derived schists.

MINE CENTRE Pae 5

The argillaceous sedimentary rocks oi the Couchiching Series underlie an area 30 miles wide to the south of Shoal Lake, but there are no exposures of Couchiching rocks on the Hanna property* Lawson 8 considered them to be the oldest rocks in the area, under* lying the Keewatin volcanics. In the Rainy Lake area this question is still unsettled, but it seems certain that the great thickness of uniform argillaceous sediments was derived from older volcanic units containing intermediate to basic flows and tuffs*

In the Hine Centre area the Keewatin volcanic rocks include felsic, intermediate and basaltic flows and pyroclastics* They occur In an easterly trending belt from 2 to 7 miles wide lying between the Quetico fault on the north and the Couchiching sediments on the south* The contact between Couchiching and Keewatin rocks is probably also a fault contact in this area.

Felsic rocks make up the greatest volume in the area between Mine Centre and Glenorchy. They vary in composition from rhyolites with more than 50& quartz to trachytic types with little quartz and a high content of light-coloured, sericitized feldspars. Fragmental lavas and tuff breccias constitute only a small proportion of the felsic volcanics, which are generally massive with distinct quarts-eyes, or fine-textured and uniform. It seems probable that a large percentage of this felsic volcanic material originated as ash flows and ignimbrite**

Relatively thin bands of intermediate tuffs and flows art interbedded with the felsic volcanic rocks, but the greatest volume of these rock types occur to the north and south of the felsic unit* Sent poorly developed pillow lavas were identified, but most of the flows are massive. Narrow felsic tuffs and soiue narrow iron formation bands occur between the intermediate flows*

SEINE i

The Seine Series comprises conglomerate and graywacke in a belt up to 4 miles wide that follows the general strike of the Keewatin volcanics* but locally shows evidence of being unconformable* In the Mine Centre area, the Seine rocks are almost entirely conglomerates, which contain a great variety of boulders and cobbles, both as to alee and rock type* Many of the boulders are granitic, but all varieties of volcanic rock are also represented. Poorly sorted boulders up to d feet in diameter are not uncommon in a matrix of graywacke that also contains rock grains of various rock-types.

POST SEINE!

The oldest intrusive unit of the area is a differentiated basic mass which forms the shores and islands of Bad Vermilllon Lake and extends west along the north shore of Seine Bay to Rainy Lake* The mass is made up of differentiated bands that vary in composition from anorthosite to peridotite. Along the northwest side of Bad Vennillion Lake, massive, lenticular bodies of titaniferous magnetite occur with anorthositic gabbro.

CENTRE Pa^e 6

Apophyses from this basic intrusive, and sill-like bodies, extend to the east of Bad Vennillion Lake within the Keewatin volcanics. When these Intrusive rocks are sheared and chloritized, they are very difficult to distinguish from the intermediate to basic volcanics.

The youngest intrusive rocks are felsic types which include granite, quartz-porphyry, syenite and pegmatite* The most prominent felsic mass is an elongated stock located between Shoal Lake and Bad Vemillion Lake. Other masses occur west of Bad Vennillion Lake end on the south shore of Bad Verraillion Lake. Most of the gold occurrences of the area are in quartz veins cutting these felsic intrusive rocks*

STRUCTURE!

The rock units described in this report are coniined by two regional, easterly-trending faults. The Quetico fault narks the north boundary, whereae a similar strong fault marks the contact between the Keewatin volcanics and the Couchiching sediments. These two faults art 8 miles apart at Seine Bay on Rainy Lake, but they converge to the East and merge at Calm Lake, just east of Flanders on the C.N.R.

The sedimentary and volcanic rock units generally trend cast- west, but in the Bad Vennillion Lake area the general strike is NSfc^, parallel to the long axis of the differentiated mafic intrusion and the granitic stocks. This change in strike is probably related to complex folding, but there is little evidence oi tops of beds in either the volcanic units or the congloirterates. Detailed capping failed to provide evidence that would unravel the complex structures that are suspected*

MffTAMORPHISM;

Most rocks of the area are affected by strong regional shearing and alteration, but these features are stronger in the softer rook units* The intrusive granites have escaped pervasive shearing and alteration although they are locaJly sheared in distinct aones.

The gabbroic iutrusives are generally massive and crystalline, but they have suffered t^ro than the granite from regional shearing, especially in the narrow sills and lenticular deposits cutting the volcanic rocks*

All of the volcanic rocks are more or less sheared and altered. The siliceous rhyolites are least affected, but most felsic volcanics are altered to sericitic schists. The andesitic and basaltic rocks have been converted to chloritic schists, but original structures such as pillows are preserved in the thick flows. Carbonate alteration has alto affected all of the volcanic rocks and the sheared gabbroic rocks* It is more intense in the very highly sheared rocks near the Quetico fault*

The congloiaeratos of the Seine Group have a fresher apptaranct than tlie volcanic rocks, but the boulders are generally elongated to some extent, and the matrix is altered by carbonatization, chloritization and sericitization.

Regional shearing is sub-parallel to the stratigraphy* It- strikes about N600E in the southwest part of the property and changes to a strike of about N800E east of line 190+OOEast. However the shearing often makes a small angle with contacts between flow units and with bedding In the graywacke bands of the Seine conglomerate.

CENTRE

GEOLOGY Of THE PROPERTY i

Geology along the bate lines and picket 3ines was mapped at a scale of l inch c 200 feet, and was plotted on 8 standard sheets of S6" X 44" size. Copies of theae maps are enclosed in a folder at the back oi this report. The general geology was e leo reduced to e scale of l inch ~ 1/4-utile, tind a copy is bound into the report.

The property was stoked to cover the extensions of the rhyolitic rocks in which zinc sulphide mineralization occurs. This mil t pinches out to the west into Seine-type conglomerate., but ,, expands to the north nnd east to roach a width oi" uore than l mile. It is bounded on the north by sheared intermediate volcanic rocks, and on the south by intermediate volcanic rocks and Seine-type conglomerate with graywacke.

One elliptical inaes of mafic rook with fragmental and tuffaceous bands is mapped ue basalt. It extends from line 312+00 to line S40+00 East, north of the 20+00 North Tie Line. The southern part of this body i s massive, vhoroae the northern part has bond* of fragmental and bedded tufaceous rocks, augijeeting that the top is to the north*

There are numerous narrow bands (up to &00 ft. wide) of intemoediate volcanic rocks interbedded with the felsic voloonice* In some cases these fine groined, sheared* chloritic rocks cut across the trend of shearing and bedding, but tnoet are conformable* tt is probable that some rocks napped as volcanic are sheared, altered intruslves equivalent in age to the gabbros of the Had Vermillion Lake area*

The band oi intermediate volcanics along the north edge of the property is highly sheared, cavbonatizod and ehloriti&ed, probably in part due to the proximity of the Quetico icult* It contains a high percentage of tuffaceous material with compositional banding that is drag folded and contorted. The main band 01 intermediate volcanic rocks to the south hns sufiered less metamorphism. Poorly formed pillows can be recognised in several places, imd there are interflow bands of felsic lava, cherty tali, and thin iron formation. This band trends slightly north of oast from line 200+00 East to line 400+00 East, but cliangee svriko to the west of line 200, trending obont S 600 West to line 60+00

Conglomerates of the Seine Group are exposed along the south edge of the property, end good exposures can be seen in the road cuts of Highway 11. The unit follows the intermediate volcanics through the change of strike at line 200+00 East, but is not entirely conformable, and may be resting on an old erosional surface*

At the west end o i the property the volcanic unite pinch out into conglomerate which seems to be folded ieoclinally into chevron-type folds* Poor evidence o; tops in the cedimcnts f.nd volcanic rocks along the south edge of the property suggest tops to the south* If these are reliable, an anticlinal axis is indicated along the south part of the lelsic volcanic band, and o synclinal axis close to the north edge of the felsic volcanic band,

MINE CENTRE Page 8

The felsic volcanic rocks include a massive, fine-grained rhyolite characterized by abundant "eyes" of quart?, up to 4 turn in diameter-, a line-grained, massive, stuicitized rhyolite; budded, cherty lull; and some fragmental material. The beet-developed iragmental rhyolite is on claim P.683 in the vicinity of the zinc sulphide itinera tion. Fragments are angular, very siliceous, and up to 6 inches in their long dimension. The matrix is yellow, siliceous and sericitized. Most of the felsic volcanic rock is the uniform quartz-eye rhyolite, which in some cases has sharp, irregular contacts with sheared, sericitized felsic volcanic. The uniiorm texture, and the well developed quartz eyes suggests that this unit may be a welded tuit or ash-flow g No original textures to coniiiu, this could be seen in thin section*

The rock mapped as quartz-gabbro is a massive, iresh-looking, dark green rock, characterized by "eyes" oi blue quartz. A good ex posure is in the railroad cut at line 264+00 East. It is a sill-like body that pinches out to the west at line 212+OOE and extends to the east boundary. J t can be traced easily because ol its high magnetic relief, but it is also well exposed in outcrop. However, at the east c-nd of the property the outcrops are so badly sheared and altered that the rock was first mapped us intermediate tui'i. Only the continuity ot high magnetic readings identities it as part oi the quartz-gabbro sill* A second narrow sill of quartz gabbro has been interpreted trow magnetic readings between lines '.'.52+00 East and line 300+00 East, south of the base line.

There are no exposures of granitic intrusive rocks on the Hanna claims.

.DESCRIPTION OF MINERALIZED AkCAS

A number o J old pits and trenches on quartz veins andstringer zones were located in the course of mapping. These apparentlydate from the 1930's when the area was last prospected tor gold.

A number oi zinc sulphide occurrences have been opened up more recently by trenching done by G. I.. lidgeon of Wabigoon. Most zinc sulphide occurrences are in patented claim l'.683, irom line 96+OOE to line llb+OOfc, but some minor occurrences are exposed In trenches on claim K.301, just north oi highway 11. Khyolitic volcanics are well exposed in outcrop on a ridge running through l'.683 to K.301, e distance of 1^ miles. Small lenticular patches a iew feet in length are stained and oxidized throughout this ridge of outcrop. These small patches are no doubt caused by disseminated sulphide mineralization. Kock trenches ere confined to the larger mineralized zones which can be measured in tens of J eel of strike length. Sphalerite occurs as a stockwork of massive stringers up to an inch thick, irregular blebs, end disseminated grains. A few grains of chalcopyrite and 2-S nan seams of pyrite also occur. The host rock is a highly siliceous, waxy-looking rhyolite breccia.

None oi the individual exposures has ore-grade material, but the extent oi mineralization and the favourable rock type makes the property an attractive exploration target.

MINE CENTRE Page 9

PREVIOU^ WORK DOME ON THE PROPERTY

There is ample evidence in the form of old trenches and pits, that the property was thoroughly prospected for gold in the period between 1900 and 1939. Some of these old pits are completely grown over with mature poplar bush.

In 1969, Kerr Addison optioned the patented claims owned by G. L. Pidgeon, and staked additional ground along strike. A program of napping and geophysical work was carried out, and aix short diamond drill holes were drilled under the surface trenches. The deepest hole was 124 feet, and the total footage in 6 holes was 672. These holes explored beneath the trenches at a shallow depth, but did not investigate possible extensions or the swamp to the south of the surface exposures. Scattered low values in cine and lead were obtained.

REFERENCES -

(1) Tanton, T. L. - Geological Survey of Canada Map 334A Mine Centre Area - 1936. l in.' if mile.

(2) Tanton, T. L. - Preliminary Report on Mine Centre Area, Ontario, G.S.C., Jan.1935.

(3) Young, W.L. - Geology of the Bennett-Tanner area, Ont. Dept. of Mines Vol.LXIX Pt 4, 1960.

(4) Map 2115 - Compilation Seriea, Ontario Dept. of Minea, 1967. "Kenora-Fort Frances Sheet" - l in. * 4 mi.

(6) Mcwilliams, G. and Ali, A. - Mine Centre-Entwine Lake Sheet - Ont. Dept. of Minea, Preliminary Map P.965 - l in. * 2 mi. - 1974.

(6) Rose, E. R. - Geology of Canadian and Vanadiferous Occurrences of Canada - G.S.C. Economic Geology Report No.27, 1973*

(7) Lawson, A.C. -The Archean Geology of Rainy LakeRe - Studied G.S.C. Mem.40 - nap no.98a-1918.

(8) Lawson, A.C. -"Report on the Geology of the Rainy Lake Region1* Annual Report, G.S.C. Vol.111, 1888 Report F*

(9) Robinson, A.H.A.1917 - "The titaniferous magnetite deposits of Seine Bay and Bad Vermillion Lake; Mines Branch Canada, Sun.Rept. p 11-22*

(10) 1922 - Titanium Mines Branch Canada, Publication No.529.

/^u

Nelson Hogg , District Geologist December 31, 1975

PROJECT AREA

UETICO

PROVINCIAL l

PARK


LOCATION MAP

MINE CENTER PROJECT


MINE CENTRE PROPERTYKENORA MINING DIVISION, ONTARIO

CLAIMS LOCATION MAPSCALE l": 1320'

KJOO SOO O 1000 2000l

Work by Dote

Interpretation Date

RevisedNTS. No. 5Z-C-IO

yfi

Quartz Gabbro - prominent blue qtz. eyesConglomerate - minor greywacke

Felsic Volcanics - Flows S tuff

Intermediate Volcanics - Includes some int

Basalt

Surface Exposure of Sphalerite

Completed Drill hole

Crone GEM ConductorApex Max-Mini Conductor

rusives


MINE CENTRE PROPERTYKENORA MINING DIVISION, ONTARIO

GEOLOGIC MAPSCALEl": 1320'

IOOO 500 O 1000 ZOOO

Work by Dote 1975

Interpretation j. Muhic Revised January, Dote November, 1975 NTS. No. 52-C-lO

•fVfV

•nliiMl-ij^jr-1 " ''"^^^^^^^V

*i;f^ Ontario52C!6SWe428 2 .2297 L ITTLE TURTLE LAKE 900

"*;.;,'- f 'K f 1 :. 1 ;

TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.MAR2PROJECTS UNIT

MAGNETICType of Survey (s) —Township or Area __Mine Centre area (Kenora")

Claim Hnlder(s) The Hanna Mining Go.

Survey Company The Hanna Mining Co.-—————-

Author of Report __John F * Muhic_______;————————— Address of Author__805 - 69 Yonge St.. Toronto. Ontario:

Covering Dates of Survey May 10.1975 -Dec.8. 1975(linecutting to office)

Total Miles of Line r..t 124.30

SPECIAL PROVISIONS CREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.ENTER 20 days for each additional survey using same grid.

DAYS per claimGeophysical

—Electromagnetic———Magnptnmpt/r 20 J

—Radiometrici———^L-—Other_________Geological.

Geochemical.

AIRBORNE CREDITS (Special provision credits do not apply to airborne surveys)

Magnetometer. .Electromagnetic. . Radiometric(enter days per claim)

DATE: Feb.12/1976 . .____-John F.MuhiC Author of Report or Agent

Res. Geol.. . QualificationsPrevious Surveys

File No. Type

V

Date Claim Holder

MINING CLAIMS TRAVERSEDList numerically

SEE ATTACHED LIST(prefix) (number)

TOTAL CLAIMS 3-2Q

GEOPHYSICAL TECHNICAL DATA

GROUND SURVEYS — If more than one survey, specify data for each type of survey

Number of Stations 367 base stations___________Number of Readings 11.685 Station interval 50 feet - 25 feet in anomalous areaS.ine spacing_____400 feet

Profile scale ____________________________________————————————Contour interval. 100 gammas

O

Instrument SCINTREX MF-2 Fluxgate magnetometer

Accuracy — Scale constant 20 gammas per scale division on the most sensitive scale

Diurnal correction method Closed loop-——————^^—^—^^-———^————^^—-—————-Base Station check-in interval (hours) Approx. 3/4 hour .———— - ' --'-________

Base Station location and value 148+OOE on base line 00_________. . , : .Value; 195 gammas

U

S Ww

Instrument

Coil configuration — Coil separation ——

Accuracy —————— Method:

Frequency—————

Parameters measured.

CD Fixed transmitter D Shoot back CD In line CD Parallel line

(specify V.L.F. station)

>O

Instrument.Scale constant.

Corrections made.

Base station value and location .

Elevation accuracy_

•rf N

W Cd(4

2

Instrument .^^^—^-^— Method l l Time Domain

Parameters — On time ^-^— Off time ^-—— Delay time ___

— Integration time.

Power.Electrode array ———

Electrode spacing —

Type of electrode _

Q Frequency Domain

_ Frequency _____

_ Range —.-—,—-^——

THE HANNA MINING COMPANYROOM BOS, 69 YONGE STREET TORONTO, ONTARIO M5E 1K3

C4i*3 ati-aoxa

LIST OF CIAIMS FOR ASSESSMENT CREDIT

K 419502K 419503

K 419505K 419506K 419507K 419508K 419509K 419510K 419511K 419512K 419513K 419514K 419515K 419516K 419517K 419518K 419519K 419520K 419521K 419522K 419523K 419524

K 419527K 419528K 419529

K 412629K 412630K 412631K 412632K 412633K 412634K 412635K 412636K 412637K 412638K 412639K 412640K 412641K 412642K 412643K 412644K 412645K 412646K 412647K 412648K 412649K 412650

MINE CENTRE PROJECT

K 412651K 412652K 412653K 412654K 412655K 412656K 412657K 412658K 412659K 412660K 412661K 412662

K 434751K 434752K 434753K 434754K 434755K 434756K 434757K 434758K 434759K 434760K 434761K 434762K 434763K 434764K 434765K 434766K 434767K 434768K 434769K 434770K 434771K 434772K 434773K 434774K 434775K 434776K 434777K 434778K 434779K 434780K 434781K 434782K 434783K 434784K 434785K 434786K 434787

K 434788K 434789K 434791K 434792K 434793K 434794K 434795

K 434797K 434798K 434799K 434800K 434801K 434802K 434803K 434804K 434805

K 412716K 412717K 412718K 412719K 412720K 412721K 412722K 412723

MMMMMW

Total - i

Ontario

Ministry of Natural Resources

GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT

TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORT,FACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT l

TECHNICAL REPORT MUST CONTAIN INTERPRETATION. CONCLUSIONS ETC.

ECEIVED

5AR2 1976

Type of Survey(s). Township or Area.

Claim Holder(s^

ELECTROMAGNETIC (C.E.M.)

Mine Centre Area (Kenora^The Hanna Mining Co.

Survey Company The Hanna Mining Co.

Author of Report ____John F. MuhicAddress of Author 805 - 69 Yonge St.. Toronto T OntarioCovering Dates of SurveyMay 10,. 1975 - Dec.8 t 1975—————

(linecutting to office)124.30Total Miles of Line Cut.

SPECIAL PROVISIONSCREDITS REQUESTED


/~, u ' i f Pcr claim \ Geophysical l| 20— Electromagnetic.1 , ,. — y

—MflgnptoTnptpr \ .S

— RaHi"'*}'*t"'1-Other

frpnlngiral.

Opnrhpmiral

AIRBORNE CREDITS (Special provision credits do not apply to airborne surveys)

Magnetometer. .Electromagnetic. . Radiometric

nATR-Feb. 12/76

(enter days per claim)

SIGNATURE: ——

i Q. O S"/ -6

Res. Geol.. . QualificationsPrevious Surveys

File No. Type Date Claim Holder

PROJECTS UNIT

MINING CLAIMS TRAVERSED List numerically


l

TOTAL CLAIMS. 120

l



Number of Stations _ 6264

Station i

.Number of R M Hing.-3*30Ha- 6264; 390Hz- 2009

100 feet, 50 feet in anomalous areas T.ine sparing 400 feet

Profile scale l" s 40_____________________________________——Contour interval.

OH M

S

InstrumentAccuracy — Scale constant . Diurnal correction method .Base Station check-in interval (hours). Base Station location and value ___

O

sw

Instrument ______Crone GEM_________ Coil configuration Horizontal Shoot Back

Coil separation 300 feet___________A * 0.5 degrees Accuracy._______— ' to———————.Method: CD Fixed transmitter

1830 Hz; 390 Hz __

W Shoot back CD In line D Parallel line


Parameters measured Dip angle of resultant field ______

O

Instrument

Scale constantCorrections made.

Base station value and location .

Elevation accuracy.

^ fc

Instrument —,———-——— Method D Time Domain

Parameters — On time ____ - Off time __

— Delay time ^——.— Integration time.

Power.Electrode array —— Electrode spacing — Type of electrode _

CD Frequency Domain _ Frequency ______ Range -^————,

THE HANNA MINING COMPANYROOM 805, 69 YONGE STREET TORONTO, ONTARIO M5E 1 K3

TCkftHOMt 141*) 9*

LIST OF CIAIMS FOR ASSESSMENT CREDIT MINE CENTRE PROJECT

Claim No419502419503

41950541950

KlT5507^| K 419508 Vt| K 419509 K 419510 K 419511/3 K 419512^

K 419515,,K 419516^ K 419517^ K 419518^

-K 419521^

K 412629^ K 412630 K 412631JI

K 412633 K 412634 K 412635K 4126364 K 412637 K 412638 K 412639 K 412640 K 412641 K 412642 K 412643, K 412644^ K 412645. K 412646*4- K 412647 K 412648 K 412649*3 K 412650'!

20'

O O34

2020

710

22020121718

3 O

16 3 O

16

OO

14

202020

O20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 10 10

KClaim No *t

412651 ^L 10Days Days

412652 412651

K 412654 K 412655 K 412656 K 412657

41265K 4126^ - K 412661/4^

CT41266J)

K 434751 K 434752 K 434753 K 434754, K 434755^ K 434756^ K 434757^ K 434758'^ K 434759VJ, K 434760)*, K 434761 K 434762 JH K 434763^ K 434764^ K 434765^0 K 434766)C K 434767 K 434768

-K 434770^ K 4 3

434772 K 434773 ,K 434774

434775JK 434776/1 K 434727^6 ~ 4 3477 XK~334"f79?g

K434781T 434781

K 434782

K 434784' 434785~434786434787

/1(K

\K

202020

O88O

20 20 20 20 15 14 12 10 13 20 20 18 10 10 10 14 18 20

O 8

12 O O O O

10 5 O 8 O O O O

13 O OO

K 4347 9TK 434792K 434793K 43479T ^K 434795^,

K 434797^K 43479854 K 4347^9^ft 434800^

[ K 434801 K 434802

43480434804'

41271^ K 412717' K 412718 K 412719 K 412720^

12721^34127J

K 412723-

578 O O O O

12 O

O13 20 20 20 10

O 10

Total - 120 Claims

Cauoxc. c| -

70y24-

Ontario

Ministry of Natural Resources


File.


TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

Type of Survey(s) ELECTROMAGNETIC (APEX)Township or Area Mine Centre Area (Kenora)Claim HnlHer( s ) The Hanna Mining Company

Survey Company Geosearch Consultants Ltd.Author of Report John F. MiihicAddress of Author 805 - 69 Yonge St.. Toronto. Ontario Covering Dates of Sn™y Sept.l6,1975-8ept.28,1975. NOV.26/7J

{linecuttingto office) to D6C.5/75.

Total Miles of Line Cut 124.30____________________

SPECIAL PROVISIONS CREDITS REQUESTED


Geophysical—Electromagnetic.—Magnetometer——Radiometric———Other—————-

DAYS per claim

See attacj-isr.

Geological.Geochemical.

bed

AIRBORNE CREDITS (Special provision credits do not apply to airborne iurveyi)

Magnetometer. .Electromagnetic. . Radiometric(enter days per claim)

- Feb.12,1976 SIGNATURE:. F.Muhi.uthor of Report or Agent

-a o?/ -tRes. Geol.. .QualificationsPrevious Surveys

File No. Type Date Claim Holder



l

TOTAL CLAIMS. 120



____________Number of Readings.Number of Stations.

Station interval __Profile scale —-—^—

2968100 feet

l" - 40^

Contour interval.

(J

iInstrument.Accuracy — Scale constant. Diurnal correction method.Base Station check-in interval (hours). Base Station location and value -———

2*68

.Line spacing. 400 feet

U Instrument

i*gO

Apex Parametrics Max**Miri 11H-4

Szq0st ftw J M

Toil rnnfigiiratinn Horizontal Loop

Coil separation 400 feet

Arrurary — 2/0 — 0

Method: C] Fixed transmitter ., CD Shoot back -6p In lineFrequenry 888 Hz


D Parallel line

Parameters measured Field strength jn ppr cent.

Instrument.

Scale constant,Corrections made.

Base station value and location ,

Elevation accuracy_

Instrument —-——.-—.—- Method l l Time Domain Parameters — On time ——

— Off time ——.

D Frequency Domain _ Frequency ______ Range .——————-

Delay time.— Integration time.

Power.

Electrode array ——

Electrode spacing — Type of electrode _

lTHE HANNA MINING COMPANY

ROOM BOB, 69 YONGE STREET TORONTO, ONTARIO M5E 1K3

t4i*j ata-aoai

LIST OF CLAIMS FOR ASSESSMENT CREDIT

K 419502K 419503


K 419527K 419528K 419529


MINE CENTRE PROJECT

K 412651K 412652K 412653K 412654K 412655K 412656K 412657K 412658K 412659K 412660K 412661K 412662


K 434788K 434789K 434791K 434792K 434793K 434794K 434795

K 434797K 434798K 434799K 434800K 434801K 434802K 434803K 434804K 434805

K 412716K 412717K 412718K 412719K 412720K 412721K 412722K 412723

~——~-

Total - i

y

File.

E i* O



TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

GeologicalType of Survey—— Township or Area- Claim holdf-r(s) The Hanna Mining Company

Mine Centre Area (Kenora")

Author of Report Nelson Hogg.Room 80S, 69 Yonge St., Toronto,Ont.M5E 1K3

Covering Dates of Snrv,,y May 10, 1975 -Oct.13.1975_______(linccutting to office)

Total Miles of Line cut 124.30____________________

SPECIAL PROVISIONSCREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.

ENTER 20 days for each additional survey using same grid.

Geophysical -Electromagnetic-—Magnetometer— RarljnmPlrif

-Othpr ffipnlnair*! ( 40

OporhfnY)irar —

DAYS per claim

r-AIRBORNE CREDITS (Special provision credits do not apply to airborne surveys)

Magnetometer. .Electromagnetic, . Radiometric(enter days per claim)

HATR- Dec.31, 1975 SIGNATURE:

PROJECTS SECTION Res. Geol. —-———— Qualifications .Previous Surveys

Checked by. .date.

GEOLOGICAL BRANCH

Approved by. .date.

GEOLOGICAL BRANCH.

Approved by. -date.

RECEIVED

FEB231976PROJECTS. .UNIT


(prefix) (number)

TOTAL CLAIMS. 120


GROUND SURVEYSNumber of Stations____________________________Number of Readings.Station interval______________________________________ -T . . 400 ft. Line spacing__________Profile scale or Contour intervals.

MAGNETICInstrument ——^——.———..—

(specify for each type of survey)

Accuracy - Scale constant — Diurnal correction method. Base station location———

ELECTROMAGNETIC Instrument—_____Coil configuration. Coil separation.—. Accuracy—————Method: C] Fixed transmitter ED Shoot back (Z3 Inline D Parallel line

Frequency_________________________________________________________(specify V.L.F. station)

Parameters measured^——————^————-————————-—-—————-——-————————-————.^-———-GRAVITY

Instrument-—^^^—-——--———-———^———^—^—-———-————.——.————-—--.-——-—.—Scale constant.Corrections made.

Base station value and location.

Elevation accuracy.-——-—-—-————-—————INDUCED POLARIZATION - RESISTIVITY

Instrument..^^^—-———..———————————.Time domain___________________________ Frequency domain. Frequency____________________________ Range——————Power^^^^—^-—---———-^——-—---——---—-——-------——--—--^-^-—----—-—Electrode array—— Electrode spacing. Type of electrode,

,*

* THE HANNA MINING COMPANYROOM BOS, 69 YONQC STREET TORONTO, ONTARIO MSC 1K3

TCLCMMHt 141*)

LIST OF CIAIMS FOR ASSESSMENT CREDIT

K 419502K 419503


K 419527K 419528K 419529


MINE CENTRE PROJECT

K 412651K 412652K 412653K 412654K 412655K 412656K 412657K 412658K 412659K 412660K 412661K 412662


K 434788K 434789K 434791K 434792K 434793K 434794K 434795

K 434797K 434798K 434799K 434800K 434801K 434802K 434803K 434804K 434805

K 412716K 412717K 412718K 412719K 412720K 412721K 412722K 412723

.M..

Total - i

HERON LAKE M.240792?45' 92-30'

48052'3Qg —

O)to sr co

LU

a:UJHccoQ.

48 0 45'—

Jj RAINY LAKE

I.R. N0.26C

__ ^_ ^ ^. l - ^ .__ ^J —— —f-=Z-m 'li ——.

K * 'K.. . 'K

403022 '4O3020 403019 .403016

4B 052'30'

COenPO CO

LU

Q LJ UJ

48045

92 045' 92 0 30

GRASSY LAKE M.2474487923

AREA OF NNy

LITTLE TURTLE LAKE

DISTRICT OF RAINY RIVER

KENORA MINING DIVISION

SCALE: 1-INCH ^ 4O CHAINS

LEGEND

PATENTED LANDCROWN LAND SALELEASESLOCATED LANDLICENSE OF OCCUPATIONMINING RIGHTS ONLYSURFACE R IGHTS ONLYROADSIMPROVED ROADSKING'S HIGHWAYSRAILWAYSPOWER LINESMARSH OR MUSKEGMINESPATENTED S.R.O.CANCELLED

o r

c.s.

Loc.L.O.

M.R.O. S.R.O.

NOTES400 Surface Rights Reservation along the shores of all lakes and rivers.

1/2 eh. allowance for Mg. CI. 1770 along the shores of Bad Vermilion Lake - M.R.O.

Areas withdrawn from staking under Section 42 of the M ining Act, R.S o.i960.{Sec.43,Rs.o.'/o)

Order No. F ile Date Dispositionlic Lands Act 1 63472

11891

W 7/76 67BS3

7/7/67

19/2/76

S. R. O.

S.R.O.

S R. O

DATf OF, ISSUE

FEB241977

SURVEYS AND MAPPING BRANCH

NATIONAL TOPOGRAPHIC SERIES 52 C 15

PLAN NO. M -2433ONTARIO

MINISTRY OF NATURAL RESOURCESSURVEYS A ND WARPING B RANCH

52C16SW(ft428 2.2297 LITTLE TURTLE LAKE 200

THUNDER BAY

r

r-- 4 8 0 4 5

AREA Of

WILDW W l h^v b^

* "— ,

DISTRICT OFRAINY RIVER

KENORA— THUNDER BAY MINING DIVISION

SCALE: 1-INCH-4O CHAINS

-LgGENP

PATENTED LAND CROWN MNO SALE ,LEASESLOCATED LANDLICENSE ,OF ,OCCUPAT(pN^MINING RKSHtS ONLY ^SUR**CE RIGHTS ONLYROADSIMPROVED ROADSKING'S HIGHWAYS ^.^RAILWAYS : ,:POWER LINESMARSH OR MUSK9SMINES ;

C.S.

Loc.

S.R,(X

NOTES

DWE OF, ISSUE

SURVEYS AND MAPPIHQ.


PLAN NO.

f N T MN

MINISTRY OF NATURAL RESOURCESSURVEYS AND MAPPING BRANCH

SaciBSWe428 2. 5237 L ITTLE TURTLE LAKE

-t"

210

920 30"

480 52' 30"—

ro ro *frOJ

LLJcr

UJ^<-J

UJ

o:ID

UJ

-J

MANION LAKE AREA M. 2406920 I5'

480 45'——

434805,434804

l 412692 l 412661 1434767 [434758 1434783 V* 1434791 l—————u — ————— — — — — — -.\Ataff3 i — —

No. 23Ihdian Reserve

-480 52' 30"

51

50

49

48

47

46

0000roCVJ

UJo:

LU

CD Q. UJX

480 45'

9^30' 920I5

WILD POTATO LAKE AREA M.2397

C487922)52C16SW0428 2.2297 LITTLE TURTLE LAKE

AREA OF

REED LAKE

DISTRICT OF RAINY RIVER

KENORAMINING DIVISION


LEGEND

PATENTED LANDCROWN LAND SALELEASESLOCATED LANDLICENSE OF OCCUPATIONMINING RIGHTS ONLYSURFACE RIGHTS ONLYROADSIMPROVED ROADSKING'S HIGHWAYSRAILWAYSPOWER LINESMARSH OR MUSKEGMINES

C.S.

NOTES

400* surface rights reservation along the shores of all lakes and rivers.

(a,) GRAVEL FILE 1 62718

(Q M .T.C. P IT 1 089^* GRAVEL FILE 1 62718

(g) M.TC. PIT 1 058

(g) GRAVEL F ILE 16799 vol.7

(gh MNR Grovel Reserve No.228, File 162718.

DATE OE ISSUE

FEB241977

SURVEYS AND MAPPING

NATIONAL TOPOGRAPHIC SERIES 52 C16

PLAN NO. |\/!

ONTARIO


LITTLE TURTLE LAKE-M.243392045'

48 045'-

N- *0^rCM

iLU

c/)-J OD

4803730

92 0 30'

403023 . 403021 4030IB

K l 418396 l 418397.....l__---

H. P. /a33 ^

H P S~*L

31H P /si32

\y

.../"'""•—

l—-.

/

•48045'

44

43

42

41'

40

39

38

K) CVJ

LjJ

oi-

oQ.

Q-l

U— 48037'30"

920 45' 44 43 42 41 40 39 38 37 36 35 34 33 319 2 0 30'

MELIN LAKE- M.2465486923

AREA O 2.2T7GRASSY LAKE

DISTRICT OFRAINY RIVER

KENORA MINING DIVISION


LEGEND

PATENTED LANDCROWN LAND SALELEASESLOCATED LANDLICENSE OF OCCUPATIONMINING RIGHTS ONLYSURFACE RIGHTS ONLYROADSIMPROVED ROADSKING'S HIGHWAYSRAILWAYSPOWER LINESMARSH OR MUSKEGMINESCANCELLEDPATENTED S.R.O.

C.S.

Loc.L.O.

M.R.O. S.R.O.

NOTES

400' surface rights reservation along the shores of all lakes and rivers.

Sand S Gravel

M T C Pit No l 2 l 2 11 "1213 " "1214

MTC Gravel Pit 1 016 Gr o v e l File. 1 70703

23798

170756

Grovel Pit No 9 88

OR ISSUE

FIB 24,977

SURVEVS AND MAPPING] •RANCH


PLAN NO. 2474ONTARIO


52C165W0428 2.2297 L ITTLE TURTLE LAKE S30

4I9

52O

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9509

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19

50

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4195

22

4195

27

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52C16SW0428 2.2297 LITTLE TURTLE LAKE

240

4126

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412632

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52C165*8428 2.2297 LITTLE TURTLE LAKE

540

on mine centre project of the hanna mining company€¦ · in 1911, a. c. lawson (1918) and in 1934...

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