AMAX EXPLORATION, INC. PROJECT 603 RESULTS OF …

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AMAX EXPLORATION, INC.

PROJECT 603

RESULTS OF EXPLORATION PROGRAM

BURNS - NOR-U URANIUM OPTION

ROBERTS TOWNSHIP

SUDBURY MINING DIVISION

ONTARIO

Timmins, Ontario October 3, 1974

Peter T. George, P.Eng., Consulting Geologist

SUMMARY

A program of geological mapping, radiometric surveying, and diamond drilling has been completed to test the economic potential of uranium mineralization that occurs on a 54 claim property in Roberts Township, Sudbury Mining Division, Ontario.

Previous work on the property consisted of trenching, diamond drilling, percussion drilling, and radiometric surveying. An anomalous zone approximately 300 feet by 1500 feet in plan area was outlined which *s underlain by low grade (0.02 to 0.03 percent U30g) uranium mineralization.

Host rocks for the mineralization are a fine grained, grey to black, thin bedded to massive argillite of Proterozoic age. The argillite contains minor lenses of quartz pebble grit and conglomerate. The mineralized zone occurs in the basal part of the stratigraphic section within 300 feet of the Archean-Proterozoic unconformity. No uranium mineral has been identified because of the very fine grained nature of the mineralization.

Geological mapping suggests that the mineralized argillite is the stratigraphic equivalent of the Mississagi Formation of the Hough Lake Group, Huronian Super Group. Mapping indicated steep dips for both the mineralized strata and the unconformity which gave the property considerable depth and tonnage potential provided a substantial width of low grade uranium mineralization could be outlined.

The results of the drilling program did not substantiate the widespread occurrence of low grade mineralization and indicated that the Archean-Proterozoic unconformity flattens abruptly beneath the showing area and limits the depth potential of that area to 100 to 150 feet. The lack of continuity of the mineralization is attributed to the depositional environment which appears to be a flood plain - delta environment with an irregular, lensoid depositional pattern.

No significant radiometric anomalies occur on the property other than that one which correlates with the main showing.

It is recommended that Amax Exploration terminate their option commitment and file all new exploration data with the appropriate government agencies.

TABLE OF

rage

INTRODUCTION .............................................. l

PROPERTY: DESCRIPTION ..................................... l

LOCATION AND ACCESS ............................. lTOPOGRAPHY ...................................... 2SERVICES ........................................ 2

PREVIOUS WORK ............................................. 2

GEOLOGICAL SURVEY:INTRODUCTION .................................... 5GENERAL GEOLOGY ................................. 5ARCHEAN ROCKS ................................... 7

Mafic metavolcanic rocks ................... 7Gabbro ...................................,. 7Polymictic conglomerate .....,.............. 9Amphibolite tuff ........................... 9Amphibolitic greywacke ..................... 9Iron formation ............................. 9Felsic to intermediate intrusive rocks ..... 10

PROTEROZOIC ROCKS ............................... 10Argillite/Siltstone ....,................... 10Quartz pebble grit ......................... 12Quartz pebble conglomerate/breccia ......... 12Polymictic conglomerate .................... 12Quartzite .................................. 12Feldspathic quartzite .'..................... 13Limestone .................................. 13

NIPISSING DIABASE ............................... 13CENOZOIC DEPOSITS ............................... 14STRUCTURAL GEOLOGY .............................. 14

Faulting ................................... 14URANIUM MINERALIZATION .......................... 15

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Page l

INTRODUCTION

The author was retained by Amax Exploration, Inc., to undertake a program of geological mapping and radiometric surveying preliminary to a program of drilling on their Burns-Nor-U Option in, Roberts Township. Sudbury Mining Division. The program was initiated on May 15. 1974 and the drill program was terminated on August 23, 1974..

A total of 5: 5 miles of linecutting (4.8 miles of baseline and 46.7 miles of grid i rnes) were compl eted on the property and geological mapping was completed over all of the property. Radiometric surveys were completed only over those parts of the property underlain by Proterozoic rocks which amounted to approximately 15of survey^. A total of 1804 feet of diamond drilling was completed by Heath and Sherwood Drilling of Sudbury, Ontario.

Mr. Robert Grant, a graduate student at Laurentian University, Sudbury, Ontario ably assisted the author throughout the program and was responsible for the radiometric survey in addition to sharing in the geological work.

PROPERTY DESCRIPTION

The property consists of JL4 contiguous. unpatentec| mining .claims which are under option to Amax Exploration, Inc., Suite 1302 : 7 King Street East, Toronto. The claim numbers and recorded holder of the claims are presented in Table 1.

PROPERTY LOCATION AND ACCESS

The property is located in the east central part of Roberts Township. Sudbury Mining Division, at approximately 46V55' North, 81 006' West. (See Figure 1)

The property is accessible by road from Capreol, Ontario north via Highway 8C6 to the National Steel Corporation Moose Mountain iron mine a distance of 12 miles", then north via a gravel' road for a distance of 6 miles. The gravel road provides complete access to the property (See Maps in pocket). Access to the gravel road is controlled by National Steel Corporation and its use must be cleared with the mine manager.

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TABLE l

CLAIM NUMBER

S 149135 to S 149140 incl.

S 153217 to S 153232 incl.

S 153599 to S 153610 incl.

S 358518 to S 358523 incl.

S 359190 to S 359192 incl.

S 359401 to S 359403 incl.

S 408084 to S 408091 incl.

RECORDED HOLDER

Amax Exploration, Inc., Suite 1302, 7 King St. East, Toronto, Ontario,

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LOCATION MAP S.rtilo "l"

Page 4

PROPERTY, TOPOGRAPHY

The property has generally low relief with local relief of 50 to 150 feet along northerly trending outcrop ridges.

Coarse bouldery till underlies much of the property with some local sand deposits.

The vegetation consists of a.mature spruce and jack pine forest with the exception of a few areas that have been cut-over in recent years. Numerous beaver dams and ponds occur along Roberts River and its tributaries and cause a few tag alder swamps in their back waters. "~~

PROPERTY, SERVICES

Mining services, labour, and supplies are available in the Sudbury District, approximately 20 miles south of the property.

.Hydro electric transmission lines are present within 4 to 6 miles of the property and the main transcontinental line of the Canadian National Railway, is approximately 1/2 mile east of the northeast corner or' the property.

PREVIOUS WORK

The earliest prospecting in the area was for gold (Gracey,JfiSI). Magnetite-bearing iron formation was discovered in the early 1900's^ approximately six miles south of the property. Development of the iron deposits was started in the mi d J 950^s by National Steel Corporation (Hanna Mining) and production of concentrate from the Moose Mountain Mine was started in 1959.

Exploration for uranium was carried out in the J 950's in the northeast part of Roberts Township in the area of Roberts Lake. Thompson J196Q1 has described the known uranium showings in the northeast part of Roberts Township.

Kindle (1932) mapped the south part of Roberts Townshipin 1931 and Meyn 0968. 19711 of the Ontario Department of Mines published geological maps and reports of Roberts, Creelman and Fraleck Townships which providec ihe most up to date and accurate outline of the distribution of the Proterozoic sedimentary rocks.

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' '"S , '' - ^^Îr'In 1968 uranium mineralization was discovered by prospectors

in the area of claim S 149137 of the property. The property was V optioned to Nordic Mines Limited in ,1968. Bayne (1968. 1969) has

described in detail the program of work completed oy Nordic Mines. The initial program consisted of geological mapping and radiometric surveying in the immediate area of the showing. Three diamond

E drill holes were spotted to test the showing. Subsequent work by t Nordic Mines consisted of 29 percussion drill holes, 2 shallow test* * shafts, and numerous trenches. The location of all drill holes, W shafts, and trenches are presented on Map Tl (1n pocket)." Averages l' of all of the Nordic Mines sampling are presented on Map 1.V1'^ ''* ' .* '.: "

* The property was acquired by Amax Exploration, Inc. in : April 1974.

GEOLOGICAL SURVEY

INTRODUCTION

^Geological mapping was started onjfoy 15. 1974 and was completed "on August 17. 1974. The complete property was mapped at a scale of l inch to 200 feet and the results of this mapping are presented on Maps 2. 3 and 4, (in pocket). The area of the main uranium showing was mapped at a scale of l inch to 40 feet and the results of the detailed mapping are presented on Map 1 (in pocket).

GENERAL GEOLOGY

The geology of Roberts Township has been described by Meyn (1971|. The township is underlain by highly deformed Archean metavoTcamc and metasedimentary rocks that have been intruded by Archean felsic and mafic igneous rocks. The Archean rocks are unconformably overlain by Proterozoic sedimentary rocks of the Elliot Lake, Hough Lake, Quirke Lake, and Cobalt Groups of the Huronian Super Group.

The Proterozoic sedimentary rocks have been folded, and block faulted which results in relatively discontinuous remnants of Proterozoic strata surrounded by Archean basement rocks. Table 2 presents the Table of Formations for the property .and the Proterozoic stratigraphic nomenclature used for the property. The stratigraphic nomenclature is based primarily on the assumption that the limestone unit that occurs in the south part of the property correlates with the Bruce Limestone Member of the Espanola Formation. The remainder of the nomenclature used is extrapolated from this datum.' '

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APPENDICES

APPENDIX l Radiometric DataAPPENDIX. 2 Drill logs and Assay data

APPENDIX 3 Assessment Work Breakdown

MAPS (in pocket)

MAP l

MAP 2

MAP 3

MAP 4

MAP 5

MAP 6

Detailed Map, Main Showing, Scale: l inch to 40 feet.

Geological Map, South Sheet, Scale: l inch to 200 feet.

Geological Map, Central Sheet, Scale: l inch to 200 feet.

Geological Map, North Sheet, Scale: l inch to 200 feet.

Radiometric Survey, South Sheet, Scale: l inch to 200 feet.

Radiometric Survey, Central Sheet, Scale: l inch to 200 feet.

DRILL SECTIONS Scale l inch to 40 feet.

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TABLE 2

TABLE OF FORMATIONS

CENOZOIC

RECENT

PLEISTOCENE

Fluvial clays and silts, swamp deposits.

Boulder till and sand deposits.

UNCONFORMITY

PRECAMBRIAN

PROTEROZOIC

NIPISSING-TYPE DIABASEGabbroic dikes and sills

INTRUSIVE CONTACT

HURONIANCOBALT GROUP.

LORRAINE FORMATIONMassive green siltstone

GOWGANDA FORMATIONThin bedded (varved?) argillite

QUIRKE LAKE GROUP: SERPENT FORMATION

Quartzite ESPANOLA FORMATION

Siltstone, greywacke, quartzite BRUCE MEMBER

Limestone BRUCE FORMATION

Polymictic conglomerate

HOUGH LAKE GROUPMISSISSAGI FORMATION

Argillite and gritty argillite, minor conglomerate.

UNCONFORMITY

ARCHEAN . ;

METAVOLCANIC- METASEDIMENTARY - GRANITIC BASEMENT COMPLEX.

Page 7

Pleistocene deposits in the area of the property consist of a very coarse boulder till which is locally overlain by fine sand deposits.

Figure 2 is a generalized geological map of the property illustrating the major lithologic and structural features.

ARCHEAN ROCKS (Map unit 1)

The Archean basement rocks on the property consist of mafic metavolcanic rocks, mafic tuffs, conglomerate-breccia, and banded- cherty, weakly magnetic iron formation. The supracrustal rocks have been intruded by gabbroic and granitic dikes, sills, and stocks. Some of the rocks mapped as gabbro may in fact be metavolcanic in origin, the coarse grained gabbroic texture probably being a contact metamorphic effect near the granitic intrusive contacts.

MAFIC METAVOLCANIC ROCKS (Map unit la)

Massive, fine to medium grained, equigranular, locally schistose, dark green rocks, consisting dominantly of chlorite, amphibole, and altered feldspars have been mapped as mafic volcanic flow rocks. Some of these rocks, particularly in the area north of line 56N may be massive mafic tuffs interbedded with sedimentary rocks and iron formation.

The mafic volcanic rocks contain up to 5# finely disseminated pyrite and are locally veined with epidote stringers. Small, barren quartz veins are relatively common.

In the vicinity of granitic intrusive contacts, the mafic metavolcanic rocks become medium to coarse grained with a gabbroic texture.

GABBRO (Map unit Ib)

Rocks mapped as Archean gabbro consists of fine to coarse grained, equigranular, dark grey to black rocks consisting of feldspar, amphibole and pyroxene. The amphibole {hornblende) appears to be fresh, occurs in laths and is probably of metamorphic origin. The feldspars are generally saussuritized. Quartz veins and epidote veins are common. The rock becomes dioritic in appearance near granitic intrusive contacts. .

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LEGENDPROTEROZOIC "i 4 Nipissing Diabase 3 Huronian Sedimentary Rocks

ARCHEAN 2 Felsic Intrusive Rocks - l Mafic Volcanic Rocks IS Amphibolitic Sedimentary Rocks IF Iron Formation

Fault

Scale l" to 2640'

FIGURE 2

Page 9 -v

POLYMICTIC CONGLOMERATE (Map unit le)

The rock is composed of pebbles of mafic volcanic rocks and some quartz vein material in a fine grained, massive to schistose, amphibolitic matrix. The pebbles are generally flattened and elongate parallel to the schistosity.

The band of conglomerate that strikes in a northerly direction from line 32N, TOW to line 52N, 7W was mapped as Proterozoic by Meyn (1965),.. The rock unit is conformable with the Archean volcanic rocKsT has an amphibolitic matrix, is cut by granitic stringers and quartz veins, and does not contain any granitic pebbles. The author considers the unit to be of Archean age.

AMPHIBOLITE TUFF (Map unit Id)

Fine grained, generally thin bedded, chlorite-biotite- amphibolite occurs in the north half of the property. The rock is probably a metamorphosed mafic tuff. Some of the masslvt amphibolite interbedded with the tuff may be volcaniclastic in origin rather than a flow rock.

AMPHIBOLITIC GREYWACKE (map unit le)

Fine grained, thin bedded arenite consisting of light grey greywacke containing laminae of black amphibolite occurs in only one outcrop located on line 112N at 13E.

IRON FORMATION (Map unit If)

Two zones of iron formation occur interbedded with the mafic tuffs and flows. The iron formation is thin bedded and dark grey-green to black with light grey chert bands. The rock is weakly magnetic, probably containing at a maximum 10/K magnetite. The rock is very similar to the "amphibolitic mafic tuff with the addition of chert and magnetite beds. .

Page 10

FELSIC TO INTERMEDIATE INTRUSIVE ROCKS (Map unit 2a,b,c)

The principle felsic intrusive rock is granitic in appearance, being a fine to coarse grained, pink, equigranular rock consisting of 10 to 25 percent quartz, 55 to 85 percent orthoclase, and 50 to 10 percent hornblende and/or biotite.

Locally the rock is probably a monzonite (2b) as the proportion of plagioclase exceeds that of orthoclase. This generally occurs near contacts with mafic volcanic rocks and probably represents contamination of the granitic magma by assimilated inclusions of volcanic rock.

Similarly, a dioritic phase (2c) occurs near some mafic volcanic contacts.

PROTEROZOIC ROCKS (Map unit 3)

Proterozoic sedimentary rocks underlie approximately~30X of the property. Correlation of these strata with other Proterozoic rocks is at best tentative however a possible stratigraphic nomenclature is indicated in Figure 3. For mapping purposes, the stratigraphy was subdivided on the basis of lithology and no stratigraphic nomenclature ahs been applied to' the geological maps.

Figure 3 presents a detailed description of the lithologic sequence along 3 sections through the property and the reader is referred to this figure for details that are not provided in the general lithologic descriptions presented below.

Meyn 11971) considered most of the gabbroic rocks in the area to be post-Huronian, Nipissing Diabase-type intrusives. Much of the gabbro is of Archean age and the area described below (Section 4) as Nipissing Diabase is probably pre-Huronian in age.

ARGILLITE/SILTSTONE (Map unit 3a)

This rock unit consists of a fine grained, massive to thin bedded lutite which ranges in colour from dark grey to grey- green to pale green. The unit is locally gritty to pebbly with quartz and quartzite grains common, and mafic volcanic and granitic grains of minor significance. Particular units can be traced along strike on the basis of colour and sedimentary structures.

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QUARTZ PEBBLE GRIT (Map unit 3bj

Quartz pebble grit units have been distinguished only when the unit was of sufficient thickness to be mapped. The rock is inequigranular and generally consists of well rounded grains of 1/8 inch to 1/4 inch white to blue-white quartz in an argillitic to arenaceous matrix.

QUARTZ PEBBLE CONGLOMERATE/BRECCIA {Map unit 3c)

Two main varieties of quartz pebble conglomerate occur on the property.

In the area south of line 28N, rounded to subangular pebbles and cobbles of white quartz and quartzite occur in a dark grey, fine grained, massive argillitic matrix which locally contains rounded to subangular fragments of argillite. This lithologic type is confined to the basal 400 feet of the stratigraphic section and would generally appear to consist of reworked sedimentary material possibly derived from an older Proterozoic unit.

In the area from line 8N, 12E tc 12N.2W the quartz pebble conglomerate consists of pebbles of massive quartz vein material in a rusty, pyritic, argillaceous greywacke matrix. This is a basal unit but does not appear to be the stratigraphic equivalent of the conglomerate described in the preceeding paragraph.

POLYMICTIC CONGLOMERATE (Map unit 3d)

Polymictic conglomerate occurs in lenses along the unconformity between the Archean basement and the Proterozoic sedimentary rocks. This basal conglomerate consists of poorly sorted pebbles and cobbles of mafic volcanic and granitic rocks in an argillaceous to sandy, dirty chloritic matrix.

Higher up in the stratigraphic section lenses and beds of polymictic conglomerate occur within siltstone and quartzite units. These conglomerates are well sorted, have a high proportion of granitic to volcanic rocks and the matrix is similar to 'the surrounding non-conglomeratic rocks.

QUARTZITE (Map unit 3e)

White to buff to grey, fine grained, massive to thick bedded quartzites are confined to the south part of the property (south of line 8N) stratigraphically above the Bruce Limestone

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Page 13

Member. Locally lenses of polymictic conglomerate occur and a few bands of argillaceous quartzite and greywacke are present.

FELDSPATHIC QUARTZITE (Map unit 3f)

North of line 40N, a major thickness of grey to white, arenite consisting of 5 to 15 percent white weathering feldspar find 85 to 95 percent quartz occurs. The rock 1s generally massive, medium grained equigranular and In small outcrops 1s difficult to distinguish from the Archean granitic rocks. Generally some argillaceous laminae may be observed in large outcrops.

LIMESTONE (Map unit 3g)

Only one limestone unit has been Identified on the property and it has been tentatively correlated with the Bruce Limestone Member of the Espanola Formation. The limestone is a white to buff, fine grained, thinly bedded, crystalline variety which locally contains minor fine-grained diopside. The limestone unit is only exposed in a few outcrops, however, a distinct airphoto lineament correlates with the limestone horizon and allows It to be traced to the south property boundary.

NIPISSING DIABASE (?) (Map unit 4)

A large outcrop area occurs as a prominent ridge between lines 4N and 28N from approximately 6E to 2W. The rock is dark grey, fine to coarse grained, massive, equigranular gabbro and consists of dark grey feldspar, amphibole, pyroxene and minor quartz. The rock weathers to a rough "knobby" texture caused by 1/4 inch to 1/8 inch clots of pyroxene and hornblende being more resistant than the feldspar.

The age of the rock is uncertain. Meyn 0971) considered it to be Nipissing Diabase of post Huronian age. Tne east contact between the gabbro and'the Proterozoic sedimentary rocks is inferred to be a fault contact. The west contact of the gabbro occurs in both Archean metavolcanic and Proterozoic sedimentary rocks. The contact with the Archean rocks is definitely intrusive, displaying a distinct chilled margin, however, the contact with the Proterozoic rocks is not obviously chilled and may in fact be an erosional surface.

The author favours the erosional contact interpretation and considers the gabbro to.be of Archean or early Proterozoic age.

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Page 14

CENOZOIC DEPOSITS

Pleistocene sediments consist of a very coarse boulder till overlain locally by sand deposits. The coarse nature of the till presents a difficult problem when sinking casing for drilling.

STRUCTURAL GEOLOGY

The property is underlain by flat to steeply dipping Archean metavolcanic and metasedimentary rocks. No top determinations were made and no fold axes have been inferred.

The Archean rocks are overlain with angular unconformity by Proterozoic sedimentary rocks. Faulting during the Proterozoic has resulted in the Proterozoic rocks in the area of the property being preserved as steeply dipping homoclinal fault blocks.

FAULTING

Three sets of faults have been inferred in the area of the property. The most prominent fault, which hos a distinct photo- lineament expression, has a north to north-northwest strike direction, displays left hand strike slip movement and the east block moved up. Related to this fault are a conjugate set of second-order faults. One fault set has an east-northeast strike direction, left hand strike slip movement and the south side moved up. The other second order fault set has a north-northeast strike direction, right hand strike slip movement and the north side moved up.

Late stage faulting along a northwesterly strike direction displays left hand strike slip movement. The dip slip direction is not known. This fault set may represent reactivation of a pre-existing Archean break. The lineament along Roberts Creek parallel to line 24N is probably an Archean fault but does not appear to have offset the Proterozoic rocks rather it appears to have been a depositional barrier and may have been a fault scarp during early Proterozoic time. "

Page 15

URANIUM MINERALIZATION

The following discussion deals with the geology of the known uranium mineralization on the property with particular reference to the area covered by Map l (in pocket). The details of exploration work completed to date are presented 1n the "Economic Geology" section of this report.

Host rocks for the uranium mineralization are grey to black, fine grained, thin bedded to massive arg1llU1c rocks containing bands and lenses of oligomictic quartz pebble grit, conglomerate and breccia. Most of the quartz pebbles are a white, fine grained, equigranular quartzite.

The Archean-Proterozoic unconformity outcrops 1n the area of line 16N at 17E and in area of line 24N at 16E. From line 8N to line 20N the unconformity has an east-northeast strike and dips to the north at approximately 65 degrees. In the vicinity of line 20N the unconformity swings abruptly to the north.

The Proterozoic strata strike in an east-northeasterly direction and parallel the unconformity along most of its length, however, in the area between lines 20N and 28N the strata generally retain their easterly strike direction and terminate abruptly against the unconformity. The unconformity in this area is probably an Archean fault scarp that stood as an erosional high during Proterozoic sedimentation.

The lensy nature of the coarse clastic rocks suggest a flood plain-delta fluvial sedimentary depositional environment. Local variations in strike and dip of the strata probably are the result of slumping and soft sediment deformation.

No uranium minerals have been identified in the argillite to date. Research work currently underway at Laurentian University in Sudbury has failed to identify the uranium bearing mineral in spite of apparently exhaustive work. The problem may lie in the grain size. Considering specific gravity differences, uraninite grains should be smaller than the associated clastic material which in this case is a fine grained argillite and at the grades involved would represent 250 to 500 parts per million of the sediment.

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i-.'ge 16

RADIOMETRIC SURVEY

\ INTRODUCTION

A Reconnaissance radiometric survey, was completed over those parts of the property underlain by Proterozoic rocks using a McPhar Model TV-4 Scintillometer, Scaler readings were made at each station utilizing a l minute counting frime. Field readings were corrected to counts per minute uranium, thorium r and potassium using the following standard equations.

u ' ( ' 3- 5 ThTh a T3"T3BkgdK - (TT) - 1.95U - 4.72 Th

The survey was performed on the following claims: S 149135 to S 149139 inclusive, S 153231, S 153232 inclusive, S 153599, S 153501, S 153602, S 153610, S 358518 to S 358523 inclusive.

A total of jj2Z-S atiflH4 were established. Field readings, corrected readings and the computer program used to perform the corrections are presented in Appendix I.

SURVEY RESULTS

Corrected readings for counts per minute uranium, thorium, and potassium are plotted on ftaps 1 r 5 and fi (in pocket). Contouring of radiometric data is highly subjective because of the masking effect of overburden which effectively prohibits the detection of radioactivity from reck buried more than a few feet.

General backgrgypd i" nvfrrjbu[ rdipni covered areas ranged from O to 30 c. p.m. uranium, In. outcrop areas, the background readings range from O to 40 c. p.m. uranium. Background is generally slightly higher in areas underlain by conglomerate.

Six anomalous areas (designated .A to F) have been outlined on.Maps 17 5 and 6. "" -

A; A broad 300 feet wide anomaly outlined by the 100 c. p. m.Uranium contour occurs between lines 12N and 24N from approximately HE on 12N to 18E on 24N. The 500 c. p. m. uranium contour outlines a zone approximately 100 feet wide by 800 feet in strike length which correlates with the main uranium showing on the property. Peak values in excess of 2500 c. p. m. occur within this area. Detailed readings indicate that the uranium mineralization occurs in particular laminae within the argil! i tic rocks. The gritty and conglomeratic units generally give lower- readings and it would appear that the

Page 17

introduction of coarse clastic material dilutes the uranium content.

Area B; A small anomaly occurs on line 64N at 5W. The underlying rock is a basal polymictic conglomerate. The anomaly is of no economic significance.

Area Cj A weak anomaly occurs between lines 8N and 12N at O to 2E. The underlying rock is a basal, rusty, quartz-pebble conglomerate. The anomaly is of no economic significance.

j\rpa H! On line 4N, from 4E to 5E a weak anomaly was obtained from argillitic rocks. The anomaly is of no economic significance.

Area JL: From line 12S to 24S at approximately 30E a moderately anomalous zone (up to 550 c.p.m. uranium) has been outlined. The anomaly is underlain by a basal argillite sequence with quartz pebble grit and conglomerate that is probably stratigraphically equivalent to the rocks underlying the main showing. This area should be further evaluated if the main showing proves to be economically viable.

3rpa f ~ A number of weak anomalies occur in a shallow overburden covered area from 16S to 24S at 9E to 18E. The anomalies are not of economic significance.

CONCLUSIONS

Only two potentially significant anomaly were outlined by the radiometric survey. AnomaVv A corresponds with the main uranium showing and indicates an anomalous zone 300 feet wide by 1500 feet long.

Anomaly E is not as strong as Anaomaly A but occurs in an area underlain by rocks that are probably stratigraphically equivalent to those underlying the main showing. This anomaly should be further evaluated if Anomaly A proves to be of economic significance.

Page 18

ECONOMIC POTENTIAL

INTRODUCTION

The economic potential of the property lies in the possibility of developing an economically viable deposit of uranium mineralization in the basal part of the Proterozoic stratigraphic section.

. Robertson and Lattanzi D974L have reviewed the geology and origin of Elliot Lake-type uranium mineralization and the reader is referred to that summary paper if he is not familiar with the exploration model for this type of 'deposit.

The sequence of events which led to the discovery of uranium on the property has been presented (See Previous Work). The detailed geology of the area of known uranium mineralization is presented on Map l and has been discussed above.

GRADE POTENTIAL

Bayne (1968. 1969) has described in detail the exploration work completed by Nordic "dines Limited in the area of the main showing.

Initial sampling of the original showing in the vicinity of line 16N at 15E gave assays of 0.215 percent U30ft over a width of 11 feet and 0.40 percent U30Q over a width of 15 feet.

Three holes (D-l. D-2 and D-3. Map 1) were drilled in October 196& to test the snowing and yielded assays from a trace to 0.04 percent U30g . Bayne J1968L concluded that the holes were not spotted accurately enough to cut the downward extension of the ore grade surface showing and also concluded that AX core was of - too small diameter to properly sample the mineralization.

Bayne (Ig68) recommended a program of .trenching, bulk sampling, and shallow percussion drilling to further evaluate the Turface showing .*

Page 19

detail:has described the results of this work in

(a) Bulk Samplings .Two .test shafts were sunk to obtain bulk samples tor assay and metallurgical testing. Shaft l is located at 16+50N, 15E and is approximately 30 feet deepl O2 ton bulk sample averaged 0.038 percent (0.76 Ibs) UÔg per ton.

Shaft 2Js located at 2H60N, 17+20E and 1s approximately 25 feet deep. A 10 ton bulk sample from this shaft averaged 0.025 percent (0.50 Ibs) ILO per ton.

(b) Trenching^ ûmerous trenches were made in outcrop and through overburden. "All of the trenches and average chip sample assays for the total length sampled are presented on Mao L Bayne (1969), presents a detailed sample plan with the individual assays. Substantial widths of low grade uranium mineralization are indicated by this sampling program.

(c) Percussion prilling; holes (numbered l .to 29on Map~T

Twejitv-nine. shallow percussion drill _ _ were drilled to test the grade

of uranium mineralization present. Table 3 summarizes the significant assay data from these holes. The assay data indicates a widespread zone of mineralization that averages 0.029 percent {0.58 Ibs) lLOft per ton. Holes l to 18 outlined an area 400 feet by 50 feet with an average drill hole depth of 20 to 30 feet and a maximum depth of 80 feet.

Bayne (1969) recognized that a very real sampling problem existed on the property because of the very fine grain size of the uranium mineralization and its apparently erratic distribution.

Comparative results from Shafts l and 2 for various sampling methods are presented in Table 4. The bulk samples produced the most representative assays whereas the percussion cuttings generally produced lower than representative assays probably because of the loss of fines in the drilling process. Channel samples could be misleading if the uranium occurs selectively in narrow bands which might be either under or oversampled.

Bavne 0969) recommended a minimum of BX core sampling - for any drilling on the property.

TABLE 3 Page 20y ANALYSIS OF TEST HOLES -ROBERTS RIVER PROPERTY - NORDIC INDUSTRIES LTD., f

INTERSECTIONS AVERAGING 0.50 LB. U 3 0g OR BETTER' i

HoleTotal Depth prill ea ' (feetT

Footage From-To

•TH-1L! TH-2 -'TH-3 . .:TK-4TK-5TK-6TK-7

! TII-0: Tii-9 ,'1 TK-10: TH-11 .

20'-.20 .202535-30'25r.o '

.7035 .70

i TH-12 8.0

TH-13 TK-14 TH-15

K'H-16 Til-17

Til-18 TH-19 TH-20

f i TK-21

f TH-22 f . TH-23

TK-24 TH-25 TH-26 TH-27 TH-28 TH-29

9090909090

90709080

9090

909035'

202090

i Total 1795 Average**

0 - 200 - 200-200 - 100-1350 -300 - 100 - 600-65

20 - 2530 - .5565.- 7010 - 1520 ,- 2545 - -SO65 - 7520 - 9060 - 850-90

30 - 350 - f.

10 - 1545 - 70.0 - 900-70

50 - 800-15

55 - 600-900-10

25 - 3560 -'9085 - 9030 - 400 - 350 - 200 -100-90

20: :: . 20:' '\20'•"10'

.x/ 1 35'-.'30; 10: 6065

' .. 5' -:'--25'•, 5-•:" : -- 5

. ''- ' . 5' 5

• ; : 10.7025- - ' - ;- !55

•- S:, 30'

•y . ~-

-' ; 30'15

' 5-

- 10' 10

30•; s10

- . - -- .10-

Seim pi e Horiz.Length *Width(feet) (feet)

20 r 20V:

10 V CO GS

.- 5 --25 '' 5.'..,

Low f, njcfh Assay in Ho lg \ Assay Minimum UÔp Maximum U^0f l

'(over .5')Maximum U- (over 5')

595 ; •19"

25

5.55

30

15- 5

10 10 30

5 10:

lo'

Ib./ton

' 0.58•;;; 0.55V 0.65 .:vo,55-:.\: Q!58 ; ; : '0.60 '-vo.r,5 -

0.50 j 0.52.. 0.60 '

' o.5o ;0.50. - 0.50.

. 0.55 v •..0.51.V

0.50 Y

0.50 O.SO 0.50 0.52

0.560.500.60

O.,51 0.50 0.52 0.60 0.60

0.50

0.55

Ib./ton -: 0.50 "-':

•'•- 0 .40 . 0.50^

V::o.3o ;-. Vo.40- v ; .- 0.30 V;'

Tr. ,' 0.40

. 0.30 , '.-•. Tr. -, ;; Tr. ••\ i ''..'

] '--:.- Tr. -v

1 Tr..Tr.Tr.

0.20Tr.

Tr..Tr.Tr.

. Tr.

Tr. •Tr.

Tr.Tr.Tr.Tr.

' Tr. -Tr.

Calculated assuming, dip of bedding 45 degrees north**Notei . ! '" ' ' " ' ; ' -' "' . -' -'.V: .'..V;--; '' -v •.-:'"'' s' .-S2±as \ , ' -; Arithmetic Average.- -'-: i '.'.v jZ^

^M^^'^^M^^^^^^fSk.'t-'--'.:. :.-- "-'.. - -:.: - l ^^.^••'^•.'•••y :-'-- : ^' - ' •:- ;'-.-' i ,. •^•.-' '•••Oc^b

Ib./ton

0.70 .'.0.7 O: o.70•-0.60•.1.00

1.10•-0.60.1.000.70

.0.50

-••vv,.'•'-'J -

:,0.60 :

1.100.800.30

.0.500.00

0.300.300.800.60

0.400.70

0.60 0.80 0.20 0.30 0.60 0.40'-

S^Bayne, P Og^rober 7th, 1969

i#-:

TABLE 4

Page 27

SAMPLING METHOD HORIZONTAL TOTAL DRY AVERAGEWIDTH WEIGHT ASSAY(feet) (tons) ( 1 U30g )

SHAFT l

1. Percussion drill cuttings Holes 27 and 28

2. Channels chipped by hand

3. Mined channel sample

4. Muck samples, hand picked

5. Bulk Sample (total mined)

SHAFT 2

1. Percussion drill cuttings

2. Channels chipped by hand

3. Bulk sample (total mined)

10

20

30

20

30

0.34

10.90

0.78

22.20

0.015

0.048

0.036

0.062

0.038

35

40

60

0.06

0.10

10

0.025

0.026

0.025

jKtfiK;,*±,r-.^'/-

t -*: t" f*'*

Page 22

TONNAGE POTENTIAL

On the basis of the current radiometric results Jj&fl—Q. and the surface trenching and sampling by Nordic Mines Limited it would appear that a potential surface area of approximately 300 feet by 1500 feet is underlain by steeply dipping Proterozoic argillites which contain widespread uranium mineralization in the 0.02 to 0.03 percent (0.4 to 0.6 l b.) UgOg range.

If the grade can be proven by drilling and if sufficientdepth can be established then sufficient volume of rock is presentto allow for a large tonnage, low grade deposit.

* *''. CONCLUSIONS AND RECOMMENDATIONS

On the basis of the work completed by Nordic Mines Limited and the geological mapping and radiometric surveying completed by the author and assistant it was concluded that the area of the main showing has potential for developing a large tonnage of low grade (0.025 percent U30g) uranium mineralization.

A drill program was started on July 9. 1974, The results of the drilling program are discussed in the following section of this report.

Page 23

DRILLING PROGRAM

INTRODUCTION

An initial program of drilling was planned to evaluate the grade, depth and strike continuity of the low grade uranium - mineralization. Three sections were planned with two holes on each section.

The holes completed are tabulated below. The program was terminated after 5 holes, were completed as the potential for a large tonnage had been eliminated.

HOLE NUMBER LOCATION ATTITUDE FOOTAGE

R-74-1

R-74-2

R-74-3

R-74-4

R-74-5

17+95N,

20+63N,

2H66N,

22+60N,

16+OON,

14+50E

9+70E

16+OOE

12+55E

10+25E

16007-450

16007-450

14507-450

14507-4501600M50

204'

435'

235.4'

402. 6'527'

Total Footage 1804.0'

DRILL PROGRAM RESULTS

Diamond drill logs and assay data are presented in, .Appendix j^ Hole' locations and summary logs are plotted on Map l and on the Dm l Sections (in pocket).

All core was split from the start of the hole to the Proterozoic-Archean unconformity.

The assay results do not indicate any substantial widths of low grade mineralization and the abrupt flattening of the unconformity severely limits the depth potential of the property.

Both factors indicate that the property has little economic potential for either a large tonnage, low grade deposit or a small tonnage, high,grade deposit.

Page 24

A possible explanation for the geometry of the unconformity is that it represents an overturned valley, the valley bottom having an easterly strike direction and a dip of 60 to 70 degrees to the north with the roll or flattening in dip representing the valley wall (See^Figure 4V.

The lack of stratigraphic correlation from one hole to the other suggests that the sedimentary units are lense-Hke. This lense-type depositional mode probably explains the lack of continuity of the mineralization with depth and along strike.

CONCLUSIONS

The exploration-work completed on the property to date has eliminated the potential for a large tonnage, low grade uranium deposit in the area of the main showing. Assay results Indicate no substantial widths of low grade mineralization and the drilling indicated that the Proterozoic-Archean unconformity flattens substantially beneath the showing, a factor which limits the depth potential beneath the main showing to 100 to 150 feet.

None *f the radiometric anomalies located during the survey would indicate the presence of other areas of uranium mineralization similar in grade to that which occurs 1n the area of the main showing.

RECOMMENDATIONS

It is recommended that Amax Exploration terminate their option on the property and file all data with the appropriate government agencies. '

Respectfully submitted,

Peter T. George, P.Eng., Consulting Geologist.

"•rrvfe'-'-V^'W'..^.'^ -"'.i- ±'-#-i:} i.Z:-ii'Zi}~*L- - .

Page 25

fi

VALUEV

A -

PRftAEMT

ORKSrIN OF STRUCTURE

-fl/v

REFERENCES

Page 26

a j i^fr..'-.t- ffi#-.\ . -'t r .'^••lv-'.'::-' - * -wA?.'.':.'-- : - ' .'

Bayne, A.S. 1968

1969

Report to Nordic Explorations Limited on the Roberts River Group of Claims and Vermillion River Group of Claims; A.S. Bayne and Company, December 1968.

Interim Wind-up Report to the President and Directors Nordic Industries Limited on Roberts River Property, Roberts Township, Sudbury Mining Division, Ontario; A.S. Bayne and Company, October 1969.

Gracey, A.H. 1897 Placer gold on Vermillion River; Ontario Bureau

of Mines, Vol. VII, pt. 3, pp 256-259.

Kindle, L.F. 1932 Moose Mountain - Wanapetai Area; Ontario Dept.

of Minos, Vol. XLI, pt. 4, pp 29-49.

Meyn, H.D.1968 Roberts Township; Ontario Department of Mines,

" Preliminary Map P449, Scale l Inch to 1/4 mile.

J971 Geology of Roberts, Creelman and Fraleck ——' Townships, District of Sudbury; Ontario

Department of Mines and Northern Affairs,Geo!. Report 91, 48p.

Robertson, D.S. and Lattanzi, C.R.1974 - Uranium Deposits of Canada; Geoscience Canada,

Thomson, J.E. 1960

Vol. l, No. 2, May 1974, pp 8-19.

Uranium and Thorium deposits at the base of the Huronian System in the District of Sudbury; Ontario Dept. of Mines, Geo!. Report l, 40p.

COMPUTER PROGRAM

SJCG WATFIV ULU,TIfC*2,PACES^50 R. GRANT GAMMA RAY

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MAPS 5 AND 6 (IN POCKET)' ' CORRECTED RESULTS OF

NCRCIC OPTION, ROBERT

MEASUREM

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' - ' -' : '

URANIUM

123

. 4 56 78 9

10 1112 13

1516 17Ifi 1920 H222324 2526 2728

LCCATICN ,..2.2SMe

22S15E 2.21X6.^.22S17E J2S16E22S19E32S2CE22S21E 22S22E2-2S24E 22S25E22S26E 22S27E22S28E 22S29E22S3CE 32S31E2ES17E 28S18E28S19E 28S2CE-28S21E 28S22E28S23E 28S24E28S25E

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NCC NOCNOC NOCNCC NCCNCCNCCNCC

15W CCNCC NCC

icvT ccNOCNOC NCCNCC NOCCC

NCCNOC NCCNOC NCCNCCNOCNOC

C 237.509.00

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-9.504.50

-4.5047.00 15.50

-10.00 -26.5018. CO 24.5017. CO -6.50

-23.50 -38.00

1.50 -10.5032.50 39.0011.50 9. CO6.50

THORIUM

C 2-3*0010. CO 1.3-00.2.00 5.000.00 4.00 11.00 7.009.00 17. CO

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f). 00 21.000.00

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POTASSIUM

CI20.0431.25 51-2637.41 21.1829.85 43.6243.30 30.4916.74 56.5415.55 41.9332.74 1.17

35.90 33.94 -31.53 68.6336.14 51.3852.04 39.1146.79 28.8321.42 24.5715.73

T 292.00

109.00 1C3.0089.00 98.0082. CC 89.00

108.00 80.00101.00 120.0077.00 70.0083.00

1C2.0083.00 86. CC103.00 83.00

1C8.00 118.0091.00 ICO.OO87.00 90.0087.00 88.0089.00

T 338.0051.00 54.0043.00 46.0041.00 45.0052.00 48.0050.00 58.0031.00 38.0049.00 44.0041.00 40.0047.00 48.0060.00 67.0048.00 54.0038.00 37.0044.00 45.0046.00

T 1151.00168.00 170.00152.00 147.00135.00 154.00176.00 117.00140.00 200.00132.00 130.00123.00 139.00143.00 149.00165.00 161.00152.00 172.00160.00 152.00168.00 158.00130.00 133.00124.00

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T 282.0063.00 65.00114.00 67.00115.00 78.0064.00 72.0082.00 68.0070.00 60.0076.00 56.00

130.00 104.0072. OC 74.0068.00 68.0092.00 92.0056.00

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tC

ASSESSMENT WORK DETAILS

Typeojtfcrvry RADIOMETRIC taiM^tlVB ' A separate fo.m i* required for each type of ti

Township or Arc fl KUBcKlS TUWNSrllr

o,?.fnn,r,,M~ AMAX EXPLORATION. INC.or Contractor Nme

SUITE 1302. 7 KING ST. EAST, TORONTOAddrew

party rhirf R. GrantName

65 Dean St.. SudburyAddrett

rYtncuiinnt P. T. GeorQeName

P f O f BQX 70. Timmins.Addrctf

ncftlooieal field mapping by,,,.N;A..iii ." " ~ Name

Addreti

COVERING DATES

IJiir rutting N.A.

F;,IH Mav 15. 1974 to June 26. 1974Instnment work, geological mapping, sampling etc.

nmr.. Auoust 15 to 20. 1974: October 6-7. 1974

INSTRUMENT DATA

M.,k. , MoHH ;,nri Typp Mcphar TV-4 Scintillometer

Sr:iir ronMant or Sensitivity 50 cun on T n over homoqeneousOr proftJr copy of instrument data from Manufacturer 'i brochure. 1 PP"I U .

K,ni;..mnri, R:.I -icfimiinH r.oimi T.J 72 T ? 65 T,j 41 cpm..

Nitmhrr "f Station* Wi*hi" Claim (JpMip — 2?'

Numhrr "f RraHinp* WMÎ-' Claim (-ronp . ...2D91

Number "f Mikf "f 1 Jn** rin Within CI --'im f^rn^p .... , ,,51*5.., ... , ,.

Num'"' r I lf S.-implrs r..i1lrrli-fl Wilhin f linn f.r.nip N.A.

CREDITS REQUESTED 20 DAYS ^0 DAYS ••-•- Include.per t Uim per cfaim (Line cutting)

Geological Survc)' D D

Geophysical Survey C Prorated D OwTkv(see 11st)

Geochemical Sur\-cy D ^ Q.-, . * jj . 4fc

PATK October 8, 197 4;ir.MKn ^^t'/C^y*^

Illllllllllllllllllllllllllllllllllll

MINING CLAIMS TRAVERSED List numerically

proratco ureoiti* S 149135 ffwiis 3

S 149136 10 ^

S 149137 12 ^ STsw.

S 149138 12 ^

S 149139 15 ^

S 153231 10 5

S 153232 12 ^~

S 153599 20S 153601 10 ^~

l/,,S,,1,5.36p2....................1.5.^..............

S 153610 8 7-y

S 358518 10 ^2

S 358519 20

S 358520 20

S 358521 20

S 358522 20 ^

S 358523 20a t Y ! ^ • rf\t\f(\ C\ CAoVvvyO/T' 0 ICov^l/i

"^^ \ i -l^ '

nx-zo -34O— (n+5),J , X,,l,,,,,,/,.

s t ^* ^ oayxT3 - — rnTAi ri /IMS 17

Send in Duplicate to:

FRED W. MATTHEWS ! , SUr-LRVISOR-PROJECrS SECTION j DEPARTMENT OF MINES k f NORTHERN AFFAIRS f t WHITNEY BljOCK \/ Qr.iEN"SPARK TORONTO, ONTARIO

2*

C

i1|iiJ

1

i S

r S|^

fPerformance and coverage credit! do not apply to airborne furveyt

v

;: ,4^'rS îlj*?-'^ Oi^Type of^wrvey^f^.;:^W-'l y^'Township or

ASSESSMENT WORK DETAILS

Geological Survey S LinecuttinqA separate form it required for each type of lurvey

Roberts Township___________

Linerntt^r I. Burns or Contractor Name

1073 Stafford St.. Sudbury, Ontario.Addrcu

?'Pafty ChiefName .

, Addreu

Name

^K^-V^ " ; ' ;-'.;-;.- :. - -- ,-"- - ,': -' Addrwi•^Geological field mapping by P.T. George-*S^-.';'i'*j '- '-V ' ' ' '. •••' ' ' ' ' " :' -: , , -. - . Name . v

P.O. Box 70y Timmins, Ontario —-- ^(jjjp,, ~~ ~"

COVERING DATES

T.ini* r.mting Apri 1 2 to June 30r 1974

May 8 to Air;ust 26. 1974Instrument work, geological mapping, sampling etc.

Office____September 9 to October 8 1 1974

j! INSTRUMENT DATA^ ,.^ t : L-J1———LI ——. l —— ... - —— - --. . -. . J

'Make, Model and Type. N.A.

N.A.Scale Constant or Sensitivity,—^—. , Or provide copy of instrument data from Manufacturer's brochure.

^Radiometric Background Count

- Number of Stations Within Claim Group

^v Number of Readings Within Claim Group

; Number of Miles of Line cut Within Claim Group

A Nur.bcr of Samples Collected Within Claim Group

N.A.

N.A.

N.A.

51.5

N.A:1

' fe CREDITS REQUESTED

fer Geological Survey.vM^jV^^-^.-fr:,.' ji/'; : , : ,":^^-spy.h '^W:'w'- ;'"'' - -

em3ckl Survey'

20 DAYS per claim

D

D

D

40 DAYS per claim

D

- Includes (Line cutting)

Show Check/

R" October 8/74 sir.NF.n

SPECIAL PROVISION CREDITSfor

PERFORMANCE fc COVERAGE

MINING CLAIMS TRAVERSED _____List numerically_____

SEE ATTACHED LIST

TOTAL CLALMS-J1

Send in Duplicate to: i '. -. V r :".-:-''-?'S.V.i.;ri;',--""FRED W. MATTHEWS :;^-t; SUPERVISOR-PROJECTS SECTION DEPARTMENT OF MINLS 8r '* NORTHERN AFFAIRS VWHITNEY BIX)CK I ^'vÛiw^^.v

;;::QUEEN'S PARK ; ^-.^d^'S^^vA^-' TORONTO, ONTARIO i^:* r^v-v

Perform*nce and cov,: - -..••'•."'.. ' •',^.'''"?s::-'t '- ~j ,i''-'' • 'y~.' f ^'^y^-^\,^f^^.^--i'-'jîy..

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SUDBURY

SUDBURY MINING DIVISION.1 'f 1

SCALE: 1-INCH-4O CHAINSr'C r^-. 1l"JTll J VIV 1 ^ Cr__3 \ls*b^ si Si"*"* V LEGEND

PATENTED LANDCROWN LAND SALELEASESLCXJATED LANDLICENSE OF OCCUPATIONMINING RIGHTS ONLYSURFACE RIGHTS ONLYROADSIMPROVED ROADSKING'S HIGHWAYSRAILWAYSPOWER LINESMARSH OR MUSKEGMINESCANCELLED

se—i?1^

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- "!* j" 1 " ifts\"^~ . * C*~ . *~ 7 1 7 3-L 1 ** 0 i X

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NOTES400 Tutfoce Rights reservolion oround o

L o kes S Rivers

. FINING UNUS DATI OF ISSUE

OCT 24 1974MINISTRY

NATURAL RKOURCB

PLAN NO.-

ne r Twp. M. 973MINISTRY OF NATURAL RESOURES

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LEGEND

PROTEROZOIC

NIPISSING (?) DIABASE

HURONIAN SEDIMENTARY ROCKS

Q Argilliteb Quartz pebble gritc Quaiiz pebble conglomerate/brecciad Polymictic conglomerate

e Quartzite

ARCHEAN

FELSIC INTRUSIVE ROCKS

a Granite

MAFIC METAVOLCANIC ROCKS

a Massive to schistose amphibolite

b Residual Soil ?

SYMBOLS

ffo 1800

NORDIC MINES, average chip sample assay, 7o U oVwidth

Radiometric reading, corrected cpm Uranium (See Appendix l)

Radiometric Anomaly^ 100,500 and iUOO cpm contours for corrected uranium.

O f r .

INSTRUMENT^ McPhar TV- 4 S cintillometer

SEE MAP 2 FOR STANDARD SYMBOLS

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20E-

MAPDETAIL WORK

MAIN SHOWING

PROJECT 603- B URNS-NOR-U URANIUM OPTION

ROBERTS TOWNSHIP ONTARIOSCALE: l inch to 40 feet NTS 41 l 14

AUGUST 1974

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