l.l.tindale 8t associates inc
TRANSCRIPT
l.L.TINDALE 8t ASSOCIATES INC.Suit* 907 -110 Erskint Avtnu* Toronto, Ontario, Conodo M4P IY4
Ttttphon* (416) 481-5761
41P11NE0409 63.5453 TYRRELL 010
INTERIM REPORT
ON THE
EXPLORATION OF THE
MATONA GOU) PROPERTY
Tyrrell Township, Ontario
FOR
ASQUITH RESOURCES INC.
November 20, 1988
Toronto, Ontario
&G - - -o
J. L. Tindale 6 Associates Inc.
snnethlW. Johnson Project/Geologist
41P11NE8409 63.5453 TYRRELL 010C
TABLE OF CONTENTS
Suntmary ' page 1.
Introduction page 2.
Property Description page 2.
History page 5.
Description of Asquith Resources' Exploration Program page 5.
General Geology page 6.
Property Geology page 7.
Results of Asquith Resources' Exploration Program page B .
Conclusions page 11.
Recommendations page 14.
Cost Estimate of the Proposed Exploration Program page 15.
Sources of Information page 16.
List of Figures and Plahs
Location and General Geological Map page 3.
Property Map page 4.
Area of Interest Map page 12.
Detailed Geology of the Sulphide Pit; 1"*5' page 13.
Geological Survey Plan; 1"*200' pocket
Detailed Geological Plan-Main Zone; I"s5' pocket
Detailed Geological Plan-Hare Creek Zone; 1"*5' pocket
Compilation Map and Proposed Exploration Program; ln*125' pocket
1.SUMMARY
Exploration of the Matona Gold Property in the 1930's traced a gold-bearing horizon over a strike extent of approximately 1400 feet, through a series of surface trenchings and underground development on two levels. Recent exploration by Asquith Resources Inc., of the surface expression of this "Main Zone" confirmed the presence of gold mineralization within this structure, and suggests that the zone remains open both at depth and along its strike extent. Further exploration by means of geophysical methods as well diamond drilling has been recommended.
This most recent exploration has also discovered a new zone of gold mineralization situated approximately 450 feet east of the Main Zone. High- grade gold mineralization has been derived from surface samplings of a north-trending, quartz-bearing shear zone. Geophysical data suggests that this zone extends further to the north over a distance of 1400 feet. Diamond drilling of the vein and its suspected northward continuation is definitely warranted.
2.
INTRODUCTION
On November l, 1988, Mr. J. L. Tindale, president of Asquith Resources Inc., 907 - 110 Erskine Ave., Toronto, Ontario, M4P 1Y4, retained the author to prepare a summary report of the Company's recent exploration program on the Matona Mine Property, located in the ShiningTree Area of the Province of Ontario. The scope of this report is to discuss the exploration methods employed during the project, the results generated, and to provide recommendations for a program of exploration to further appraise the economic potential of the property.
The program of exploration on the Matona property was completed during the period of August to October 1988, under the supervision of the author. This report is based on the results of that program, as well as research of available data pertaining to the project area.
PROPERTY DESCRIPTION, LOCATION, ACCESS, AND TOPOGRAPHY
The ShiningTree Area straddles the boundary between the Districts of Sudbury on the west and the Timiskaming District on the east.
Access is provided via Highway 560 which connects the village of ShiningTree with the villages of Gowganda and Elk Lake to the east, and Westree to the southwest. Further to the west, the junction of Highway 560 and 144 provides all-weather access to the cities of Sudbury and Timmins.
The Matona Gold Property is comprised of 19 leased and contiguous mining claims situated in the northwestern section of Tyrrell township. The claims cover 791.04 acres and are numbered as follows: G.G.5843 to G.G.5851 inclusive, G.G.5957 to G.G.5965 inclusive, and G.G.6273. Access to the leases is provided along a bush road extending south from Highway 560, just east of a high-voltage transmission line, approximately 17 miles west of the village of Gowganda. Logging roads extending off of the main bush road provide excellent access to all sections of the property.
Topographically, the area consists of south-trending depressions characterized by swampy creek-beds, surrounded to both the east and west by north-trending ridges rarely exceeding 100 feet in relief. Overburden generally consists of outwash deposits which can vary in thickness from 5 to 100 feet. Vegetation is mixed second growth comprised predominantly of alders, birch and poplar along with stands of black spruce and cedar. The southeastern-most section of the property has been cleared by logging operations and is covered with a thick growth of poplar seedlings.
LEGEND
MATACHEWAN TYPE DIABASE
NIPISSN6 TYPE INTRUSIVE DIABASE
HURONIAN SEDIMENTS
FELSIC INTRUSIVE ROCKS
METASEOIMENTS
FELSIC METAVOLCANICS
INTERMEDIATE S MAFIC METAVOLCANICS
LOCATION MAPSCALE ! l ^ 64 MILES
LOCATION a GENERAL GEOLOGICAL MAP
SHININGTREE AREA
SUDBURY 8 TIMISKAMING DI STRICTS,. ONTARIO
SCALE: i"* 4 MILES SEPT., 1981
IfDECKER PROPERTY ? TYRANITE PROPERTY
MCINTYRE PROSPECT
MIS XT7 MOS \ 8 MOKNIGHT TWP.
TYRRELL TWP.
MATONA PROPERTY
SLOANE
M 1 G. CO. LTD. ?SOKOLOFF?
MINTO PROPERTYFOXDALE
^MINES™ Brttzt
PROPERTY MAP
KNIGHT S TYRRELL TWPS
DISTRICT OF TIMISKAMING , ONT.
SCALE : l" s '/2 MILE SEPT., 1081
MAP NO. 2.
5.
HISTORY
The history of the area has been well documented by Rennick, M.W. (1988). In short, gold was first discovered in the ShiningTree area in 1911. Numerous gold discoveries followed, and in 1930 claims were staked to cover a gold-bearing shear zone located in the northwestern corner of Tyrrell township. Under the Matona Mining Syndicate the gold-bearing shear was tested through a series of trenches and eight short diamond drill holes totalling 1,249 feet. All the holes cut the vein structure, and in 1935 underground development of the structure was inaugurated..
By 1937 two drift levels were established at the 125 and 215 foot horizons through a two compartment shaft completed to a depth of 231 feet. One raise to surface from the 125 foot level was completed as well as drifting and crosscutting on both levels amounting to 1623 feet. Only limited work was completed on the 215 foot level but the downward continuance of the vein structure was confirmed.
In 1946, seven drill holes were completed totalling 3,007 feet in the area of the shaft which also confirmed the downward extension of the vein structure.
From 1946 onwards there has been little or no exploration on the property. Several parties had attempted to arrange financing for re- evaluation but were not successful in their efforts.
DESCRIPTION OF ASQUITH RESOURCES' EXPLORATION PROGRAM
Asquith Resources completed this reported surface exploratory program during the period of August 10 to October 20, 1988. The program consisted of approximately 23 miles of linecutting, generating picketed grid lines with 100 foot station-intervals. The individual lines were spaced at 200 foot intervals over the central portion of the property, and 400 foot spacings over the most northerly and southerly extensions of the property. All grid lines were cut both to the east and west off a centrally located, north-trending baseline.
A magnetic survey was completed over the land portion of the grid utilizing a GEM Systems GSM-8 proton field magnetometer with an absolute accuracy of V- l gamma. A GEM Systems base station recorder was used to monitor and correct for diurnal drift of the magnetic field during the survey .
A VLF electromagnetic survey was also completed over the land portion of the grid utilizing a CRONE Radem VLF-e.m. receiver, and transmitter stations located in Cutler, Maine and Annapolis, Maryland.
Stripping of the overburden covering the Main Zone of
6.
mineralization north and west of the Matona shaft was initiated on September 12, 1988. A D-7 Catepillar tractor was first used to clear the surface vegetation from the Main Zone as defined by the old surface trenchings. A John Deere 650 excavator-type back-hoe was then utilized to scrape the bedrock clean of all soil deposits. The bedrock then exposed was washed with water using a Wajax Mark-4 fire pump. This same procedure was also carried out over an series of trenches 450 feet east of the shaft, immediately west of Hare Creek. In all approximately 41,000 square feet of bedrock was exposed and washed for detailed mapping and sampling purposes.
All exposed areas were surveyed into a detailed reference grid which was tied into grid-line locations at regular intervals. On the Main Zone of mineral izaton at the Matona shaft a reference line was surveyed along the axis of the mineralized zone with iron bars being placed at 50 and 100 foot intervals, these points being leveled with respect to the shaft elevation of 0.00 feet. The exposures along the western edge of Hare Creek were tied into a survey line trending at N200W. Both the Main and Hare Creek reference lines have been surveyed to a common point located 55 feet northwest of grid point 0+00 B.L.
Detailed geological mapping of the Main Zone and Hare Creek zone was completed on October 15, 1988 at a scale of l inch to 5 feet. Rock-saw sampling of both zones was then carried out with 229 samples being cut from the Main Zone and 70 samples being taken from the Hare Creek Zone. Blasting of the bedrock at regular intervals along the Main Zone was also carried out so as to provide a "fresh" exposure of the mineralization for sampling.
Systematic mapping of the property geology was also completed concurrent with the work noted above. All outcrop exposures and topographic features were mapped at a scale of l inch to 200 feet over the land portion of the grid area. Seventeen rock samples were sent for analysis from various areas on the property to test for additional areas of gold mineralization.
GENERAL GEOLOGY
The geology of the ShiningTree Area has been described by several authors including M.W. Rennick (1988) who summarized previous investigations as follows:
"The basement rocks of the district are separated into three main divisions: the Keewatin volcanics, the Timiskaming volcanics and sediments, and the granitic intrusives. These rocks underlie the Cobalt sediments which cover the eastern edge of Tyrrell township and the northeastern two- thirds of Knight township."
"The Keewatin rocks consist mainly of massive andesite and basaltic lavas. The Timiskaming series consists mainly of rhyolite and trachyte flows, tuff, and volcanic breccia grading up into slate, arkose, and conglomerate. Both series have been intruded by masses of granite, quartz porphyry and felsite, lamprophyre dikes, and diabase sills and dikes."
The early Precambrian metavolcanic-metasedimentary sequence are tightly folded about arcuate northwest-trending axes. These rocks exhibit a well developed foliation which trends in either a N300w direction or an east-west direction, the latter being the better developed. The Proterozoic Cobalt sediments are generally flat-lying and exhibit concordant relationships with the intrusive diabase sills.
Two directions of faulting is evident throughout the ShiningTree camp. East-west trending fault structures are the most common and generally occur as zones of shearing, and are important economically as a host of gold mineralization. North to northwest trending fault structures appear to post-date the east-west faulting, and form the regional fault pattern of the area.
PROPERTY GEOLOGY
The Matona Gold Property is predominantly underlain with a thick sequence of andesitic flows and pillowed lavas generally trending NIS^W to N400W. The unit is typically fine grained, dark to medium green in colour, moderately chloritic and foliated. Pillows are most readily evident in the western section of the property and are rarely distorted, exhibiting a younging direction to the southeast. Felsic metavolcanics are rarely exposed, and again occur to the west of Hydro Creek. Comprised predominantly of quartz and sericite, the unit is typically strongly schistose, white-brown in colour and often contains minute disseminations of pyrite along the schistosity planes. Due to the rather fissile nature of the unit, outcrop exposure is very limited and hinders the lateral projection of the unit during the mapping procedure.
Immediately south and west of B.L.0+00 lies a series of dikes or flows of trachybasalt. These rocks are fine to medium grained, aphanitic, porphyritic, dark purple to mauve rocks which show north-trending compositional banding. This north-trending, semi-comcordant body of rock appears to off-set the surrounding rock units, and is thought to have been emplaced along a pre-existing, north-trending zone of weakness.
A small lense of granite is exposed in the southeastern corner of the Matona property and is characterized by a pink or pinkish brown colour. Most commonly the granite is medium grained and occassionaly contains altered clots of ferromagnesian mineral and/or epidote.
Most conspicuous though, are the north-trending diabase dikes which form ridges of up to 50 feet throughout the property. These rocks are typically fresh, black rocks of fine to coarse grain depending on the width
8.
of the dikes. They are commonly magnetic, containing very fine disseminations of magnetite ranging to 51 by mode. Veins, stringers and irregular growths of epidote are often noted throughout the outcrop areas. The dikes are generally 100 to 200 feet wide, the widest being exposed along the hydro-electric powerline extending through the western portion of the property.
RESULTS OF ASQUITH RESOURCES' EXPLORATION PROGRAM
Detailed mapping of surface exposure along the Main Zone of gold mineralization on the Matona property has indicated the presence of a strong structural and stratigraphic control of the gold mineralization.
Approximately 650 feet of strike length along the Main Zone was exposed during the course of the program, and indicated that the main lead within the zone was comprised of a black, highly schistose and slatey horizon. Thin section analysis by Dr. G. Wilson (1988) indicates that the zone is comprised of minute platelets of graphite within abundant carbonate (calcite) and V quartz^ all constituents comprising 951 of the rock by mode. ~~
This graphitic horizon extends from the shaft striking N450W and dipping 750 to the west, and after a strike extent of 250 feet swings sharply to the northwest striking NSS^ at 750 southwest. The zone as exposed is not consistent in its strike orientation, rather it is sinuous in its nature, this being caused largely by the constant bisection of mafic intrusive dikes within the zone itself. Wilson analyses the dike as a highly carbonatized rock cut by brittle fractures which are lined with chlorite and filled with coarse calcitic carbonate. Typically fine grained and black, Wilson suggests that its mineralogy is consistent with a mafic- ultramafic protolith (lamprophyre).
The footwall of the graphitic horizon is not localized as one distinct rock unit. In the area of the shaft, a fine to medium grained and siliceous rock forms the footwall unit, and itself is not affected by the intrusive dikes which constantly bisect the graphite horizon. Largely comprised of quartz and feldspar, the rock appears to be highly altered as indicated by the presence of abundant quartz and secondary sericite. Scattered, strained quartz eyes appear to be relict phenocrysts. Wilson describes this unit as a highly altered felsic porphyry. Approximately 270 feet northwest of the shaft an agglomeratic or brecciated intrusive is emplaced between the graphitic zone and its accompanying dikes, and the highly altered felsic porphyry described above. The unit is characterized by a fine grained black matrix which incorporates large bomb-sized fragments of the hangingwall porphyry and smaller fragments of black chert. These chert fragments were presumably derived from concordant lenses of lean, cherty iron formation which occurs within the graphitic horizon itself. Up to 51 finely disseminated pyrite is exhibited within this unit, and where brecciated, carries significant values in gold.
Wilson indicates that the intrusive breccia unit consists largely of carbonate (601) and serpentine (311) with quartz as a minor constituent. The feldspathic nature of the rock suggests a matrix that is basaltic in composition. The occurrence and position of this intrusive is important economically in that the occurrence of quartz veining within the graphitic horizon is more prevalent in this area, and sampling indicates that the occurrence of gold within the horizon is likewise enhanced.
The hangingwall of the zone is comprised of a laterally distinct unit described by Wilson as a metabasalt (andesite). The carbonatized nature of the rock indicates the pervasive occurrence of calcite throughout the area as a whole.
Detailed sampling of the surface exposure along the Main zone indicates very low grade gold mineralization accompanies the graphitic horizon extending from the shaft area to an area 350 feet northwest of the shaft. Values ranging from 0.001 oz.per ton gold over 1.0 feet to 0.068 oz. per ton gold over 4.0 feet were obtained from channel samples across the graphitic horizon. The rather low assay values obtained directly reflect the lack of quartz veining (less than 11) within the graphitic horizon in this area.
Quartz veining becomes more prevalent within the graphitic slates just 40 feet southeast of the 125-level raise to surface, situated 390 feet northwest of the shaft. Lensoidal, white crystalline quartz veining exhibits widths of up to 0.8 feet and lengths of up to five feet, and occur as fracture-filling deposits within the graphitic shales. Pyrite mineralizaton in concentrations of up to 51 are evident along the vein selvages, and while not evident in the field, fine free gold occurs within the vein quartz itself, as indicated through reassay of individual vein samples. Significant gold values obtained in the area of the raise are as follows:
SAMPLE NO. COORDINATE ASSAY VALUE SAMPLE WIDTH
2201 145 NW 0.285 oz/ton Au 2.3 feet2204 155 NW 0.067 oz/ton Au 4.0 feet2205 160 NW 0.063 oz/ton Au 5.0 feet2207 177 NW 0.166 oz/ton Au 5.0 feet2209 185 NW 0.239 oz/ton Au 4.0 feet2211 195 NW 0.494 oz/ton Au 1.0 feet2217 210 NW 0.179 oz/ton Au 2.0 feet2220 225 NW 0.049 oz/ton Au 4.0 feet2223 230 NW 0.203 oz/ton Au 3.0 feet
The above noted samples represent a zone of continuous gold mineralization over a strike distance of 90 feet, and yields a weighted gold average of 0.146 oz/ton Au. over a width of 3.2 feet. This zone of gold mineralization appears to correspond well with both the No.110 and No.108 zones outlined on the 125 foot level. Samplings by L.B. Wright in 1937 averaged 0.13 and 0.15 oz./ton Au. over widths of 4.3 and 4.2 feet for these zones respectively.
10.Superimposing the surface survey plan upon that of the 125 foot
level indicates that at least 100 feet of mineralization has been outlined beyond that exposed on surface, which extends under heavy overburden cover to the northwest. Geological mapping and geophysical surveying indicates the presence of a east-west trending fault zone with left-lateral fault displacement lying immediately north of the Main Zone of gold mineralization. This fault, has in turn,been displaced by a major right- lateral fault zone trending north-northwest along Hydro Creek. It is thought that these faults have displaced the northwestern extension of the Matona Main Zone further to the north and west. The discovery of a small outcrop of lean, cherty iron formation (L12Nx2800W) which is similar to that found within the Matona Main Zone 2800 feet to the southeast, seems to support this hypothesis. Further exploration efforts will have to confront this possibility.
Stripping along a zone 450 feet east of the Matona shaft has outlined a narrow zone of gold mineralization associated with a sheared zone containing brecciated crystalline quartz veins. The vein structure reaches widths of up to 3.0 feet, and is characterized by up to 201 angular fragments of white crystalline quartz hosted within a medium grained, granular groundmass of quartz and calcitic carbonate. The shear structure strikes at N100W and dips near to vertical, and lies between sheared and carbonatized andesites to the west and a series of narrow (less than 20') dikes of trachybasalt. The vein breccia extends northwards under the cover of overburden, and to the south extends under the new road and out towards the swamp of Hare Creek. Four channel samples taken across the vein structure at ten foot intervals along strike assayed as follows:
(Individual samples taken from north to south)
COORDINATE ASSAY VALUE SAMPLE WIDTH
0+24 south 0.009 oz/ton Au 3.0 feet0+35 south 0.059 oz/ton Au 1.5 feet0+45 south 0.386 oz/ton Au 1.5 feet0+55 south 0.634 oz/ton Au 4.0 feet
This vein structure, termed the North Hare Creek Zone, is unlike any discovered to date on the Matona property, as it occurs within a different geological environment than that of the Main Zone which lies 450 feet to the west. Trenching done previous^ on a lense of black chert just 10 feet west of the vein exposure failed to test this new vein structure. The fact that it does lie near to this black cherty iron formation may prove that this new discovery is somehow tied geologically to the Matona Main Zone, in that this cherty formation is very similar to that found within the Main Zone itself, and is similar again to the exposure discovered within the northwestern corner of the property.
Magnetic and electromagnetic surveys completed recently suggest that the North Hare Creek Zone extends further to the north than that exposed on surface. A strong VLF-e.m. anomaly coupled with a weakly flanking magnetic response suggests a northerly extension to the zone of
11roughly 1400 feet. As this northerly extension of the zone lies under heavy overburden cover, diamond drilling of this anomaly will have to be completed to test its gold-bearing potential.
Stripping of the overburden 600 and 800 feet south of the North Hare Creek Zone, along a linear trend of previous trenching sites, uncovered a number of zones of shearing and carbonate alteration. Short, lensoidal bodies of sulphide (pyrite) mineralization within these sheared zones yielded gold values ranging from 0.002 oz./ton over 1.0 feet, to 0.153 oz./ton over 3.0 feet. While not of the same structure and strike extent, the occurrence of gold within these sulphide zones indicates a preferred association between gold and sulphide mineralization.
Stripping along the trend of the Central Hare Creek Zone indicates that gold can also be localized within quartz veins. Values up to 0.143 oz./ton Au. over 3.5 feet were derived from channel sampling of short, lensoidal fracture-filling crystalline quartz veins.
Sampling of a zone of heavy sulphide mineralization 300 feet south of the Central Hare Creek Zone yielded values as high as 0.785 oz./ton Au over a width of 2.0 feet. This zone, which has seen considerable amounts of trenching and pitting in past years, possesses a similar footwall and hanging wall assemblage as that of Matona's Main Zone. Although quite lensoidal in its configuration, this "Sulphide Zone" warrants diamond drilling to test the structure at depth.
CONCLUSIONS
Recent exploration of the Matona Gold Property by Asquith Resources Inc. confirmed the presence of significant amounts of gold mineralization within a structure known as the Main Zone. Underground exploration of this zone in the 1930's outlined a zone of persistent gold mineralization associated with crystalline quartz veins within carbonaceous, graphitic slates. The mineralization outlined underground corresponds well with a zone of mineralization outlined on surface in the recent program. Both the surface and underground exploration indicates that the zone extends further to the northwest, beyond what is presently outlined, this northwestern extension quite possibly being faulted to the north and west as outlined through the recent exploration efforts. Further exploration is definitely required to extend and define this mineralization both along strike to the northwest, and at depth.
Significant occurrences of gold have also been encountered along a trend known as the Hare Creek Zone. Values ranging to 0.634 oz./ton Au. over 4.0 feet have been derived from a zone of intense quartz brecciation. The southern extension of the zone extends under the cover of Hare Creek , while its northern extension has been traced through geophysics for some 1400 feet. Diamond drilling of this zone is warranted to test its economic potential.
1988 SURFACE GOLD ZONE
1936 GOLD ZONE
DRILLING A , MSECTION
MATONA MINEDEVELOPMENT AREA 382/1-5
p-634/4-Oj
153/3-0 143/3-5'
0-785/4-0
HARE CREEK ZONE
'.LEGEND
a?85X4-0' Au ox /Ion l F t
ASQUITH RESOURCES INC.TYRRELL TWP., ONTARIO
MATONA MINE PROPERTY
MILE
13.
LEGEND
3. Lamprophyre
2. Sulphide Zone
1. Andesite
DETAILED GEOLOGY
OF THE
SULPHIDE ZONE
Vi
1 inch to 5 feet
14.
Lenses of sulphide mineralization were found to contain significant concentrations of gold mineralization along a north-south trend from the North Hare Creek zone. Values up to 0.79 oz./ton Au. over narrow widths have been obtained from recent channel samplings. Diamond drilling to test the lateral extension of this mineralization should be contemplated.
RECOMMENDATIONS
The following exploration program is recommended to test the economic potential of the Matona Main Zone and the Hare Creek Zone.
1. The establishment of cut and chained grid lines extending in a north-south direction from L0+00, and westwards along this baseline from L0+00 X 6+00W, the lines to be cut on 200 foot centres with stations established at 100 foot intervals.
2. Stations should be established over those areas of swamp cover which were not suitably covered during the summer months by geophysics. All new grid stations should be accurately extended from the existing grid lines at both Hare and Hydro Creeks. VLF-e.m. and magnetic surveys should be completed over these line extensions.
3. An induced polarization survey should be completed over the newly cut north-south grid lines, as well as the east-west lines extending between the western edge of Hydro Creek and the eastern edge of Hare Creek. It is expected that the northwestern extension of the Matona Main Zone will be delineated through this geophysical method.
4. Diamond drilling of the targets described within this report is to be carried out as follows:
TARGET ZONE LINE DEPART. AZMUTH COLLAR LENGTH
Hare Creeknorth ext. 800N 400W 0900 -450 350 feet
88-2 Hare Creeknorth zone 400S 100W 0900 -450 350 feet
88-3 Hare Creeknorth zone 600S 100W 0900 -450 350 feet
88-4 Sulphide Zone 1525S 075W 0750 -450 350 feet
88-5 Main Zone 200S 800W 0350 -450 350 feet
88-6 Main Zone 200S 800W 0350 -600 400 feet
88-7 Main Zone 150S 875W 0350 -450 350 feet
DDH t
88-8
88-9
88-10
TARGET ZONE
Main Zone
Main Zone
Main Zone
LINE
150S
075S
075S
DEPART.
875W
950W
950W
AZMUTH
0350
0350
0350
COLLAR
-600
-450
-450
15.
LENGTH
400 feet
350 feet
400 feet
The above noted program represents 3,650 feet of diamond drilling. An additional 1,350 feet of drilling is to be allocated towards additional targets which may be generated through the completion of the proposed geophysical surveys, or those generated during the course of the diamonddrill program.
The proposed exploration program is expected to require two months to complete, at an exploration expenditure of $ 140,000.00 CAN.
COST ESTIMATE OF THE PROPOSED EXPLORATION PROGRAM Matona Gold Property
1. linecutting; a total of 3.5 linemiles @ 6400.00x*nile $ 1,400.00
2. Geophysical surveys: i) VLF-e.m. and magnetic surveysover areas not previously covered; total of 3.0 linemiles @ 0150.00/^1le per survey. 900.00
ii) A total of 7.5 linemiles of induced polarization surveying over both the proposed north-south grid, and the central portion of the main grid; total of 10 days at $l,250.00/day 12,500.00
3. Diamond drilling; a total of 5000 feet of B.Q. core drilling @ 623.00 per foot; includes supervision, sample preparation and storage, assays, labour and accomodation/board. 115,000.00
4. Contingency (V-8%) 10,200.00
TOTAL COST OF PROGRAM 6140,000.00
November 20, 1988 J. L. Tindale fc Associates Inc. Toronto, Ontario
inetn IN. Johnson Project/Geologist
16.
SOURCES OF INFORMATION
CARTER, M.W.1977: Geoscience Report 152, O.M.N.R.
Geology of MacMurchy s Tyrrell Townships Districts of Sudbury (t Timiskaming
RENNICK, M.W.1988: Report of the Matona Gold Property
Tyrrell Township, ShiningTree Area District of Timiskaming, Larder Lake Division Ontario; revised from Sept. 1981 report Asquith Resources Inc., May 1988 Private Placement Memorandum; confidential file.
WILSON, G.1988: Minerology of Hand Specimens from the
Matona Project, Tyrrell Twp., ShiningTree District, North-Central Ontario. Asquith Resources files.
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41P11NEe489 63.5453 TYRRELL
SUMMARY REPORT
ON THE
EXPLORATION OF THE
MATONA GOLD PROPERTY
Tyrrell Township, Ontario
FOR
ASQOTTH RESOURCES INC.
020
March 20, 1989
Toronto, Ontario
J. L. Tindale 6 Associates Inc.
Keflneth/W. Johnson Project/ Geologist
tlP11NE84B9 63.5453 TYRRELL 020C
TABLE OP CONTENTS
L
Summary page 1.
Introduction page 2.
Property Description, Location, Access k Topography page 3.
History page 5.
Description of Asquith Resources' Recent Exploration page 5.
General Geology page1 7.
Property Geology page 7.
Results of Asquith Resources' Exploration Program page 8.
Conclusions page 12.
Sources of Information page 13.
Appendix: Diamond Drill Records, Holes M88-1 to M88-21 page 14.
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List of Figures and Plans
Location and General Geological Map {figure 1) page 3.
Property Map (figure 2) page 4.
Geological Plan; scale 1"*200' (figure 3) map folder
Compilation Map and Survey Plan of Diamond Drilling(figure 4) map folder
Diamond Drill Sections of the Main Zone Si Hare CreekZones; scale I"s50' (figure 5? set of 14 sections) map folder
I.P. Pseudosections: 6W through 10W S. 18W through 30W. s Set of 10 sections;scale 1"-100'; (figure 6) map folder
V.L.F.-electromagnetic Survey Plan; Set of 2 plans; profiles and field strength plans; scale l"-200' (figure 7) map folder
Magnetic Survey; scale I"s200' (figure 8) map folder
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SUMMARY
Exploration of the Matona Gold Property in the 1930's traced a gold-bearing horizon over a strike extent of approximately 1400 feet, through a series of surface trenchings and underground development on two levels. Recent exploration by Asquith Resources Inc., confirmed the presence of gold mineralization within this structure through surface samplings and diamond drilling. Although the structure was found to be laterally persistent within the exploration area, gold values were generally of low grade. However, the lateral continuity of the horizon provides potential for additional gold mineralization in that the northwestern strike extension of the structure appears to lie some 2000 feet northwest of the mine workings.
Gold mineralization along a trend known as the Hare Creek Zone is closely associated with both quartz-carbonate shear zones, and with graphitic shales similar to those found within the Main Zone. Exploration by Asquith Resources Inc. has indicated that poor lateral continuity exists between the individual gold-bearing zones within the Hare Creek area. Further exploration utilizing advanced geophysical methods combined with diamond drilling is warranted.
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2.
INTRODUCTION
On March 9, 1989, Mr. J. L. Tindale, president of Asquith Resources Inc., 907-110 Erskine Avenue, Toronto, Ontario, M4P 1Y4, retained the author to prepare a summary report of the Company's recent exploration on the Matona Mine property, located in the ShiningTree Area of the Province of Ontario. The scope of the report is to discuss the exploration methods employed during the project, the results generated, and to provide recommendations, if any, for a program of exploration to further assess the economic potential of the property.
This latest program of exploration on the Matona property was a continuation of the program completed in October 1988, which was subsequently outlined in a report titled "Interim Report on the Exploration of the Matona Gold Property, Tyrrell Township, Ontario; dated November 20, 1988 by J. L. Tindale S Associates Inc. of Toronto. This most recent program was completed during the period December 5, 1988 to February 4, 1989, under the direct supervision of J. L. Tindale P.Eng. This report is based upon the results of that program, as well as research of available data pertaining to the project area.
PROPERTY DESCRIPTION, LOCATION, ACCESS, AND TOPOGRAPHY
The ShiningTree Area straddles the boundary between the Districts of Sudbury on the west and the Timiskaming District on the east.
Access is provided via Highway 560 which connects the village of ShiningTree with the villages of Gowganda and Elk Lake to the east, and Westree to the southwest. Further to the west, the junction of Highway 560 and 144 provides all-weather access to the cities of Sudbury and Timmins.
The Matona Gold Property is comprised of 19 leased and contiguous mining claims situated in the northwestern section of Tyrrell Township. The claims cover 791.04 acres and are numbered as follows: G.G.5843 to G.G.5851 inclusive, G.G.5957 to G.G.5965 inclusive, and G.G.6273. Access to the leases is provided along a bush road extending south from highway 560, just east of a high-voltage transmission line, approximately 17 miles west of the village of Gowganda. Logging roads extending off the main bush road provide excellent access to all sections of the property.
Topographically, the area consists of south-trending depressions characterized by swampy creek-beds, surrounded to both the east and west by north-trending ridges rarely exceeding 100 feet in relief. Overburden generally consists of outwash deposits which can vary in thickness from 5 to 100 feet. Vegetation is mixed second growth comprised predominantly of alders, birch and poplar along with stands of black spruce and cedar. The southeastern-most section of the property has been cleared by logging operations and is covered with a thick growth of poplar seedlings.
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L E G E N D
MATACHEWAN TYPE DIABASE
t l NIPISSNG TYPE INTRUSIVE DIABASE
l * l HURONIAN SEDIMENTS
j * j FELSIC INTRUSIVE ROCKS
l l METASEDIMENTS
FELSIC METAVOLCANICS
l l INTERMEDIATE a MAFIC METAVOLCANICS
LOCATION MAP
LOCATION a GENERAL GEOLOGICAL MAP
SHININGTREE AREA
SUDBURY a TIMISKAMING D l STRICTS,. ONTARI O
SCALE: i"" 4 MILES SEPT.; 1981
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DECKER PROPERTY ? TYRANITE PROPERTY
MCINTYRES7.Z9/"'"
PROSPECT
TYRRELL TWP V
MATONA PROPERTY
SLOANE
NT G. CO. LTD. ?SOKOLOFF?
MINTO PROPERTY FOXDALE^MINES
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PROPERTY MAP
KNIGHT 8 TYRRELL TWPS
DISTRICT OF TIMISKAMING , ONT.
SCALE l l" * '/2 MILE SEPT., 1981
MAP NO. 2.
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HISTORY
The history of the area has been well documented by Rennick, M.W. (1988). In short, gold was first discovered in the ShiningTree Area in 1911. Numerous gold discoveries followed, and in 1930 claims were staked to cover a gold-bearing shear zone located in the northwestern corner of Tyrrell Township. Under the Matona Mining Syndicate the gold-bearing shear was tested through a series of trenches and eight short diamond drill holes totalling 1,249 feet. All of the holes cut the vein structure, and in 1935 underground development of the structure was inaugurated.
By 1937 two drift levels were established at the 125 and 215 foot horizons through a two compartment shaft completed to a depth of 231 feet. One raise to surface from the 125 foot level was completed as well as drifting and crosscutting on both levels amounting to 1623 feet. Only limited work was completed on the 215 foot level but the downward continuance of the vein structure was confirmed.
In 1946, seven drill holes were completed totalling 3,007 feet in the area of the shaft which also confirmed the downward extension of the vein structure.
From 1946 through 1988 there has been little or no exploration on the property. Several parties had attempted to arrange financing for re- evaluation but were not successful in their efforts.
In August of 1988, Asquith Resources Inc. initiated a surface exploratory program consisting of linecutting, geophysical and geological surveying, topographic surveying, mechanical stripping and bedrock sampling in an effort to locate and define the gold-bearing zones developed during the previous programs of exploration. Approximately 41,000 square feet of bedrock was exposed by stripping in two separate areas of the property, from which almost 300 rock samples were cut which in turn outlined two separate zones of gold mineralization. Geophysical data generated during the course of the program indicated possible.lateral extensions of these zones and provided the basis for further exploration efforts on the property (J.L. Tindale Se Associates Inc., Nov. 20, 1989).
DESCRIPTION OF ASQUITH RESOURCES' RECENT EXPLORATION PROGRAM
Based upon recommendations set out in a report by J. L. Tindale Si Associates Inc., Asquith Resources Inc. completed a total of 8,022 feet of diamond drilling during the period December 5, 1988 to February 4, 1989. The drilling was contracted to McKenzie Drilling Limited of Timmins, Ontario who used a Longyear Super-38 wireline diamond drill utilizing B.Q.-sized drilling tools which yield rock-core !7Xi6 inches'in diameter. The rock- core on retrieval was placed in trays capable of holding 20 linear feet. The individual trays were then labeled and the rock lithologies logged and recorded with respect to their down-hole footages (in feet), Mineralized
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sections of core were split and sent for analysis in Kirkland Lake at Accurassay Laboratories Ltd. The remaining core trays were then transported for storage on the property at a site along the bush road 400 feet north of the shaft.
The individual hole locations were spotted with respect to their grid coordinates, and surveyed for direction using a Brunton compass. After drilling, the hole locations were marked with a wooden plug, and its position surveyed into a detailed reference grid which had been tied into grid-line locations at regular intervals. Drill holes southwest of the Matona shaft were surveyed to iron bars which had been placed along the zone of mineralization during the previous detailed mapping program. All holes were levelled for elevation with respect to the shaft elevation of 0.0 feet. The drill holes east of Hare Creek were tied into a survey line which had been placed along the trend of the mineralization at roughly N20^W. Both the Main and Hare Creek reference lines have been surveyed to a common point located 55 feet northwest of grid point 04-00 B.L.
A total of 21 holes were drilled testing two areas of mineralization, namely the Matona Main Zone and the Hare Creek Zone. The drill hole locations and total lengths are tabled as follows:
HOLE TARGET GRID COORDINATES AZMUTH ANGLE AT HOLE NUMBER ZONE in feet _____ COLLAR LENGTH
M88- l HARE C. 8+00N x 3+00W 090 o -45 o 300 feetM88- 2 HARE C. 4+50S X 0+65W 070 o -45 o 300 feetM88- 3 HARE C. 4+50S x 0+65W 070 o -60 o 450 feetM88- 4 HARE C. 4+95S X 0+50W 070 o ~45 o 350 feetM88- 5 HARE C. 15+14S x 1+00E 082 P -45 o 350 feetM88- 6 HARE C. 15+14S x 1+00E 082 o -60 0 448 feetM88- 7 MAIN Z. 8+15W x 3+15S 025 o -45 0 350 feetM88- 8 MAIN Z. 8+15W x 3+158 025 o -60 o 451 feetM88- 9 MAIN Z. 8+90W x 2+70S 025 o -45 o 350 feetM88-10 MAIN Z. 8+90W x 2+70S 025 o -60 o 446 feetM88-11 MAIN Z. 9+30W x 2+25S 025 o -45 o 350 feetM88-12 MAIN Z. 9+30W x 2+25S 025 o -60 o 450 feetM88-13 MAIN Z. 10+70W x 1+80S 025 o -45 o 340 feetM88-14 MAIN Z. 10+70W x 1+80S 025 o -60 o 449 feetM88-15 MAIN Z. 12+00W x 1+15S 025 0 -45 0 147 feetM88-16 MAIN Z. 12+00W x 1+15S 025 o -60 o 450 feetM88-17 HARE C. 14+65S x 0+85E 082 o -60 o 450 feetM88-18 HARE C. 15+62S x 1+05E 082 o -60 o 450 feetM88-19 HARE C. 13+60S x 0+13E 082 o -60 o 500 feetM88-20 HARE C. 10+30S x 1+47E 082 o -45 o 350 feetM88-21 HARE C. 7+40S x 1+30E 082 o -45 o 291 feet
Coincident with the drilling program, a limited geophysical survey utilizing the induced polarization technique was completed over the Main Zone exposure and its speculated western extension. Approximately 3.5 linemiles of I.P. was carried out along north-south lines cut at 200 foot intervals over the trend of the zone. However, the presence of an open- water swamp along Hydro Creek severely limited the coverage of the survey.
OM88 - 6 - L - 053
ADDENDUM TO SUMMARY REPORT ON THE EXPLORATION OF THE MATONA GOLD PROPERTY, TYRRELL TOWNSHIP, ONTARIO FOR ASQUITH RESOURCES INC. BY K. W. JOHNSON, PROJECT GEOLOGIST - dated March 20, 1989
Geophysical Surveys
A test line of S.P. survey was run across the known exposure of the
Matona Mine Zone to determine if the Zone could be picked up with this relatively
simple instrument. The Zone has a high carbonaceous content, graphitic in
part, and though previous VLF - EM surveys did not respond, the S.P. gave a
pronounced effect, encouraging the Company to attempt to trace the Zone west
ward under suspected deep overburden utilizing the I.P. technique as a quide
to drilling. Brief details of the I.P. survey appear on pages 6 and 7 of the
report by K. W. Johnson.
The S.P. survey utilized porous pots at 50 foot spacing intervals and
a simple voltmeter, all supplied by Crone Geophysics.
The I.P. instrumentation consisted of a Scintrex IPR - 8 receiver and a
Scintrex IPC - 9, 200 watt transmitter, owned by Claridge-La Rose Geophysics
of Bracebridge, Ontario.
MINISTRY OF NORTHER" OEVEIOPMEHT MID
OCT 1 3
incentives OFFICE
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Ten cross-sections of Time Domain I.P, were traversed using an "a"-spacing of 100 feet in a dipole-dipole potential array, and utilizing a delay time of 240 Ms. The resultant readings were presented in three parameters as resistivity (ohm-feet), chargeability (milliseconds), and metal factor (l).
GENERAL GEOLOGY
The geology of the ShiningTree Area has been described by several authors including M.W. Rennick (1988) who summarized previous investigations as follows:
"The basement rocks of the district are separated into three main divisions: the Keewatin volcanics, the Timiskaming volcanics and sediments, and the granitic intrusives. These rocks underlie the Cobalt sediments which cover the eastern edge of Tyrrell Township and the northeastern two- thirds of Knight Township."
"The Keewatin rocks consist mainly of massive andesite and basaltic lavas. The Timiskaming series consists mainly of rhyolite and trachyte flows, tuff, and volcanic breccia grading up to slate, arkose, and conglomerate. Both series have been intruded by masses of granite, quartz porphyry and felsite, lamprophyre dikes, and diabase sills and dikes."
The early Precambrian tnetavolcanic-metasedimentary sequence are tightly folded about arcuate northwest- trend ing axes. These rocks exhibit a well developed foliation which trends in either a N30^W direction or an east-west direction, the latter being the better developed. The Proterozoic Cobalt sediments are generally flat-lying and exhibit concordant relation ships with the flat-lying diabase sills.
Two directions of faulting is evident throughout the ShiningTree camp. East-west trending fault structures are the most common and generally occur as zones of shearing, and are important economically as a host of gold mineralization. North to northwest trending fault structures appear to post-date the east-west faulting, and form the regional fault pattern of the area .
PROPERTY GEOLOGY
The Matona Gold Property is predominantly underlain with a thick sequence of andesitic flows and pillowed lavas generally trending NIS^W to N400w. The unit is typically fine grained, dark to medium green in colour, moderately chloritic and foliated. Pillows are most readily evident in the western section of the property and are rarely distorted, exhibiting a younging direction to the southeast. Felsic metavolcanics are rarely exposed, and again occur to the west of Hydro Creek. Comprised predominantly of quartz and sericite, the unit is typically strongly
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schistose, white-brown in colour and often contains minute disseminations of pyrite along the schistosity planes. Due to the rather fissile nature of the unit, outcrop exposure is very limited and hinders the lateral projection of the unit during the mapping procedure.
Iirmediately south and west of B.L.0+00 lies a series of dikes or flows of trachybasalt. These rocks are fine to medium grained, aphanitic, porphyritic, dark purple to mauve rocks which show north-trending compositional banding. This north-trending, semi-concordant body of rock appears to offset the surrounding rock units, and is thought to have been enplaced along a pre-existing, north-trending zone of weakness.
A small lense of granite is exposed in the southeastern corner of the Matona property and is characterized by a pink or pinkish-brown colour. Most commonly the granite is medium grained and occasionally contains altered clots of ferromagnesian mineral and/or epidote.
Most conspicuous though, are the north-trending diabase dikes which form ridges of up to 50 feet throughout the property. These rocks are typically fresh, black rocks of fine to coarse grain depending on the width of the dikes. They are commonly magnetic, containing very fine disseminations of magnetite ranging to 5% by mode. Veins, stringers and irregular growths of epidote are often noted throughout the outcrop areas. The dikes are generally 100 to 200 feet wide, the widest being exposed along the hydro-electric powerline extending through the western portion of the property.
RESULTS OF ASQUITH RESOURCES' EXPLORATION PROGRAM
Exploration of the Matona property has indicated the presence of strong structural and stratigraphic controls of the gold mineralization.
Detailed mapping of the Main Zone previous to the diamond drilling stage indicated that the main lead within the zone was comprised of a black, highly schistose and slatey horizon. Thin section analysis by Dr. G. Wilson (1988) indicates that the zone is comprised of minute platelets of graphite within abundant carbonate (calcite) and V-quartz, all constituents comprising 95% of the rock by mode.
This graphitic horizon extends from the shaft striking N450W and dipping 750 to the west, and after a strike extent of 250 feet swings sharply to the northwest striking N650E at 750 southwest, The zone as exposed is not consistent in its strike orientation, rather it is sinuous in its nature, this being caused by the constant bisection of mafic intrusive dikes within the zone itself. Wilson analyses the dike as a highly carbonatized rock cut by brittle fractures which are lined with chlorite and filled with coarse calcitic carbonate. Typically fine grained and black, Wilson suggests that its mineralogy is consistent with a mafic-ultrattaf ic
j protolith (lamprophyre).
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The footwall of the graphitic horizon is not localized as one distinct rock unit. In the area of the shaft, a fine to medium grained and siliceous rock forms the footwall unit, and itself is not affected by the intrusive dikes which constantly bisect the graphitic horizon. Largely comprised of quartz and feldspar, the rock appears to be highly altered as indicated by the presence of abundant quartz and secondary sericite. Scattered, strained quartz eyes appear to be relict phenocrysts. Wilson describes this unit as a highly altered felsic porphyry. Approximately 270 feet northwest of the shaft an agglomeratic or brecciated"intrusive is emplaced between the graphitic zone and its accompanying dikes, and the highly altered felsic porphyry described above. The unit is characterized by a fine grained black matrix which incorporates large bomb-sized fragments of the hangingwall porphyry and smaller fragments of .black chert. These chert fragments were presumably derived from concordant lenses of lean, cherty iron formation which occurs within the graphitic horizon itself. Up to 51 finely disseminated pyrite is exhibited within this unit, and where brecciated, carries significant values in gold.
Wilson indicates that the intrusive breccia unit consists largely of carbonate (601) and serpentine (311) with quartz as a minor constituent. The feldspathic nature of the rock suggests a matrix that is basaltic in composition. The occurrence and position of this intrusive is important economically in that the occurrence of quartz veining within the graphitic horizon is more prevalent in this area, and sampling indicates that the occurrence of gold within the horizon is likewise enhanced.
The hangingwall of the zone is comprised of a laterally distinct unit described by Wilson as a metabasalt (andesite). The carbonatized nature of the rock indicates the pervasive occurrence of calcite throughout the area.
Detailed sampling of the surface exposure along the Main Zone indicates very low grade gold mineralization accompanies the graphitic horizon extending from the shaft area to an area 350 feet northwest of the shaft. Values ranging from 0.001 oz. per ton gold over 1.0 foot to 0.068 oz. per ton gold over 4.0 feet were obtained from channel samples across the graphitic horizon. The rather low assay values obtained directly reflect the lack of quartz veining (less than 11) within the graphitic horizon in this area.
Quartz-carbonate veining becomes more prevalent within the graphitic shales just 40 feet southeast of the 125-foot level raise to surface, situated 390 feet northwest of the shaft. Lensoidal, white crystalline quartz-carbonate veining exhibits widths of up to 0.8 feet and lengths of up to five feet, and occur as fracture-filling deposits within the graphitic shales. Pyrite mineralization in concentrations of up to 51 are evident along the vein selvages, and while not evident in the field, fine free gold occurs within the vein quartz itself, as indicated through reassay of individual vein samples. Gold values obtained in the area of the raise range in grade from 0.049 oz. per ton gold over 4.0 feet to 0.494 oz. per ton gold over a width of 1.0 foot. Continuous values within this assay range were obtained over a strike extent of 90.0 feet, and yield a weighted gold average of 0.146 oz. per ton over an average width of 3.2 feet.
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The recent drill program tested the northwestern strike extension of the Main Zone, and again found gold to be closely associated with quartz- carbonate alteration of a cherty, graphitic iron formation. This alteration however, was found to be quite discontinuous both laterally and at depth, occurring generally as thin lenticular stringer veinlets concordant within the graphitic shales. Gold values encountered in drill holes immediately northwest of the mine workings graded as follows:
HOLE NO. ASSAY (OZ./ton) SAMPLE WIDTH ( feet)
M88-7 0.044 14.8 feetM88-8 0.104 4.0 feetM88-9 0.100 4.1 feet
Holes M88-10 thru 16 intersected the northwestern strike extension of the graphitic formation and exhibited little to no quartz-carbonate alteration and only anomalous values in gold. Further drilling along the northwestern strike extension of the formation was hampered by the presence of the Hare Creek floodplain. The occurrence of a postulated fault trending north-northwest along Hare Creek further complicates the lateral projection of the gold zone.
Induced polarization surveying was successful in outlining the axis of the Main Zone in the area immediately northwest of the mine workings, yielding a strong chargeability anomaly combined with resistivity lows. This anomaly remains well defined through L10W and into the heavy overburden cover of Hare Creek, where no coverage with I.P. could be completed. West of the Creek the I.P. results appear to have been affected by a complex of diabase dikes which trend northwards through the northwestern quarter of the property. Weakly anomalous I.P. results are evident coincident with the flanks of the diabase intrusives. At station L30W x 12N an area of strong chargeability readings and broad-low resistivities was outlined coincident with the presence of an outcrop of lean, cherty iron formation, similar to that found within the footwall of the Main Zone. This anomaly, although it only occurs on the one survey line, is significant in that it establishes the presence of what could be the western extension of the Main Zone, and hence carries significant exploration potential.
Detailed mapping and sampling in an area 450 feet east of the Matona shaft outlined a narrow zone of gold mineralization consisting of brecciated, crystalline quartz-carbonate veins within a shear zone exhibiting heavy iron-carbonate alteration. This shear structure strikes N100W and dips near to vertical, and lies between sheared and carbonatized andesites to the west and a series of narrow (less than 20') dikes of trachybasalt. Four channel samples taken across the vein structure at ten foot intervals along strike assayed as follows:
COORDINATE ASSAY VALUE SAMPLE WIDTH
0+24 south 0.009 oz/ton Au 3.0 feet0+35 south 0.059 oz/ton Au 1.5 feet0+45 south 0.386 oz/ton Au 1.5 feet0+55 south 0.634 oz/ton Au 4.0 feet
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This vein structure, termed the North Hare Creek Zone was tested with three diamond drill holes (figures 4 fi 5). Holes M88-2 and 3 tested the zone at the 120 and 210 foot horizons and encountered a zone of rather intense quartz-carbonate shearing within trachybasalt flows. No significant gold values were obtained in this sampling. Hole M88-4 located 50 feet south of the previous two holes intersected the zone at the 100 foot level and exhibited minor pyrite in a quartz-carbonate breccia zone. Again no gold values were obtained.
Magnetic and electromagnetic surveys previous to the above- mentioned drilling outlined a north-trending, linear anomaly which appeared to be the northern strike extension of this gold-bearing shear. Drill hole M88-1, located on L8N x 3W, tested this anomaly and found the source to be a 15 foot wide annealled fault zone within massive trachytes. No gold values were obtained from this "recent" fault zone, although a short section of quartz veining along a trachyte-gabbro contact yielded an assay of 0.044 oz. per ton gold over 1.0 foot.
Drilling in the area of the "Sulphide Pit", 1000 feet south of the North Hare Creek Zone, established the presence of a new zone of gold mineralization. Drill holes M88-5 and 6 were designed to test a thin leader of massive sulphide mineralization which was extensively trenched during the 1930's. This sulphide zone was intersected in both holes, with hole M88-6 yielding assay results of 0.04 oz per ton gold over 3.0 feet and 0.09 oz. per ton gold over 3.7 feet in continuous samplings. Further downhole, a zone of intense quartz-carbonate alteration was encountered within massive trachytic flows which yielded gold values of up to 0.085 oz. per ton over widths of up to 2.6 feet. Hole M88-17, drilled 100 feet to the north intersected the same zone of carbonate alteration at the 325 foot level and assayed 0.227 oz. per ton gold over a core width of 3.5 feet. Hole M88-19, drilled still further to the north by 100 feet intersected the zone again at the 350 foot level and yielded 2.4 feet grading 0.048 oz. per ton gold. Hole M88-18, drilled 100 feet south of 88-5/6 failed to intersect any values within the zone and exhibited poor stratigraphic correlation with the holes further to the north, this most likely being due to folding and/or faulting of the section further to the east.
Hole M88-20 was*drilled 500 feet north of the Sulphide Pit and again intersected the carbonate shear zone at the 180 foot level. No gold values were obtained in the sampling of the carbonate shear, but further downhole a narrow sequence of graphitic iron formations and porphyry intrusives yielded values ranging from 0.09 oz. per ton gold over 2.0 feet to 0.417 oz. per ton over 0.8 feet. An intersection further up-hole assayed 0.182 oz. per ton gold over 2.6 feet, again associated with graphitic iron formation and porphyry intrusives. The presence of gold within this geological setting is of particular importance in that the gold mineralization found within the Main Zone is hosted within graphitic shales and associated with felsic porphyry intrusives. The geological similarity between the gold mineralization comprising the Main Zone and that found at Hare Creek may indicate that these two gold-bearing structures are strati- graphically the same unit, and have been displaced from one-another by faulting and/or folding. Further exploration ventures on the Matona property should be designed so as to test this hypothesis.
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CONCLUSIONS
Exploration of the Matona Gold Property by Asquith Resources Inc. confirmed the presence of gold mineralization within a structure known as the Main Zone. Underground exploration of this zone outlined persistent gold mineralization associated with crystalline quartz-carbonate veins hosted within carbonaceous, graphitic shales. The mineralization outlined corresponds well with a zone of mineralization defined on surface in Asquith's recent program. Surface and underground sampling combined with diamond drilling indicates that the zone extends further to the northwest, but appears to be of low grade in gold. The presence of a similar geological setting to that of the Main Zone, some 2000 feet to the northwest, indicates potential for additional gold mineralization, and definitely warrants further exploration efforts.
Significant occurrences of gold have also been encountered within both crystalline quartz-carbonate veins and graphitic shales, along a trend known as the Hare Creek Zone. Values ranging to 0.634 oz. per ton gold over 4.0 feet have been derived from quartz-carbonate breccia zones. Such zones of gold mineralization have been encountered along the entire trend of the Hare Creek Zone and generally appear to be of narrow widths and discontinuous configurations. The presence of gold-bearing graphitic shales similar to that within the Main Zone have been encountered south of the North Hare Creek Zone. Although generally narrow in width, high-grade gold values have been indicated through drilling, where the last hole of Asquith's program yielded an assay value of 0.417 oz. per ton gold over a
i width of 0.8 feet. Poor stratigraphic correlation from hole-to-hole .indicates complex structural relationships, a problem which may be resolved through the expansion of the induced polarization survey-coverage further south and east in any future exploration endeavours.
Respectfully Submitted,
March 20, 1989 J. L. Tindale and Associates Inc. Toronto, Ontario
Kennfeth W. Johnson Pronect Geologist
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SOURCES OF INFORMATION
CARTER, M.W. 1977:
JOHNSON, K.W. 1988:
RENNICK, M.W. 1988:
tL WILSON, G.
1988:
Geoscience Report 152, O.M.N.R.Geology of MacMurchy s Tyrrell TownshipsDistricts of Sudbury and Timiskaming
Interim Report on the Exploration Program of the Matona Gold Property, Tyrrell Township, Ontario., for Asquith Resources Inc., Asquith Resources' File
Report of the Matona Gold PropertyTyrrell Township, ShiningTree AreaDistrict of Timiskaming, Larder Lake DivisionOntario; revised from Sept. 1981 reportAsquith Resources Inc., May 1988 Private PlacementMemorandum; Confidential File.
Mineralogy of Hand Specimens from the Matona Project, Tyrrell Township, ShiningTree District. North-Central Ontario. Asquith Resources' File
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FOOTAGEDESCRIPTION
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DIAMOND DRILL RECORDHOLE N
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DESCRIPTION v
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EGO RESOURCES LIMITED
MATONA PROJECTOF
ASQUITH RESOURCES INC. DRILL SECTION
facing north
J. L. Tl NDALE Q ASSOCIATES INC.
SECTIOH'ISSOS
r— i— r~" r~" r
DIAMOHD DRILL RECORDNAME OF PROPERTY
HOLE NO.
LOCATION
LATITUDE
ELEVATION *- 2O*
STARTED
- VA
FOOTAGE DIP AZMUTH FOOTAGE DIP AZMUTHHOLE HO. SHEET NO.
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FOOTAGEDESCRIPTION
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EGO RESOURCES LIMITED
MATONA PROJECTOF
ASQUITH RESOURCES INC DRILL SECTION
facing north
J.L.TINDALE 8 ASSOCIATES INC.
M88-I7-- 095x14655
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HARE CREEK
SURVEY PLAN OF DIAMOND DRILLINGMatona Mine Property
Tyrrell Tp.,Ontario, CAN. scale-r-501
vertical projection ofdiamond drill M*, fi gold volu**(o j. X ion) ft mwl* width (f MI).
survey pointe, l 'iron bar
f r oad
HYDRO CREEK
North txttntion of tht North Hart Crttk
PROPERTY LOCATION
Halt
Anomaly (w*qk,|trona.)
._.x
U88-I9'19.91 LI400S
j Me? - uew
ASQUITH RESOURCES INC.
MATONA MINE PROPERTY NORTHERN PORTIONTyrrell Twp., Ontario
COMPILATION MAP
**M*tf kr K-W J.
Prawn fey; i.T. M
D*li Movtmbtr I9M
Scctoi l iiOO
Qwg Mo.To accompany a report by:
J.L.TINDALE 4 ASSOCIATES INC.
1 11'MNI W-llrVi c, i '..|i, i i YK'K'I l l200
l*, itl Hill, H.
L20N
LI6N
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L BS
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L 20 S
L22S
L 24 S
L26S
L28S
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: -. la
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SYMBOLS
Outcrop. . . . . . . . . . . . .
Geological boundary. . .
Trench , pit . . . . . . . . . . '——* *Q
Foliation , strike S dip. . —"-*
Bedding , strike a dip. . . -1-
Pillows , top shown . . . . . ~^~
Vegetation boundary... — — — —
TOPOGRAPHY
/
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LEGEND
MAFIC INTRUSIVE HOCKS
7 a - Diabase7b - Diabase , granophyric 7c - Diabase, porphyritic 7d -Olivine diabase
FELSIC TO INTERMEDIATE INTRUSIVE ROCKS
Ga - Quartz porphyryGb - Quartz - feldspar porphyryGc- Granite, massive, fi ne to medium grained6d - Aplite6e - Syenite
ULTRAMAFIC INTRUSIVE ROCKS
5a - Serpentinite5b - Diorite bc - Gabbro
METASEDIMENTS
4a - Chert4b - Sulfide iron formation4c - Oxide iron formation4d- Argillite4e - Greywacke4f - Arkose
FELSIC METAVOLCANICS
3a - Flows , massive3b - Flows , porphyritic , oliated3c - Tuff
INTERMEDIATE METAVOLCANICS
2o - Flows , massiveZb ~ F lows , pillowed2c - Tuff2d - Agglomerate
MAFIC METAVOLCANICS
la - Flows , massive , fine - medium grainedIb - Flows , massive , coarse grainedle - Pillowed flowsl d - Flows , porphyriticl e - Flows , foliatedIf - Tufflg - AmphiboliteIh - Chlorite schisth - Flows , silicified , carbonotizedl j - Pillowed brecciaIk - Trachyte.
\-t-A-
x \
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v
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m
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L 42
O 100 200 300 400 bOOft.r ..l
ASQUITH RESOURCES INC.
MATONA MINE PROPERTYSHINING TREE GOLD AREA
Tyrrell Twp., Ontario
GEOLOGICAL PLAN
|^,'y.'"l,t l. K.W.
?.TM.
Dot*. November 1998
Scale-, (inch- 200ft.
Dwg. No.
L 46S \
/
/^
T lo
;1
7f1
——— 1 —————————————
\ i limit of\ clear- cut
areai
\1 \s\\
\\
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l \
black spruce\ black spruce a muskeg ' 6 e :
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black spruce a muskeg
1\1\
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-a*y 2o,sn.' breccia
l ion* w. pyl 6 lT,F*C0 3
\
second - growth poplar * *
S
s
(lean)
i,*.g
To accompany a report by:
J.L.TINDALE 4 ASSOCIATES INC.
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1 11' l INI (Sllfl'l li.l '.'I'll l Yk'k'l l l 210
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36 L
lot
ASQUI1H RESOURCES INC
SURVEY
SoLD
TWR,A R EA } O N 7.
l" ' 20)'
J.L . W DAL ASSOCIAES C.
LE G E KJ D
-L -J
ab w
30
lot
24-0
9 , dk , purple
B.L.OOS10 CM
0.009/3.0 a . * f .
Trench
o7s3V4?o : sheared
^ . . 7 Q *1^—— crystalline qtz ^"x " . \ f ragments
,: w fuchite
35W
GEOLOGICAL LEGEND
\
in CM00
Tr./S.O
9 Trachyte dykes
SYMBOLS
— Geological contact, observed
Shearing
8 Crystalline quartz veins
Iron- carbonate shear zone
6 Cherty - breccia zone
o.ooi/i.sT S am P|e "iterval; l oz/ton Ati/widtl* iin feet 5 Graphitic sediments
Sulfide iron formation
Porphyritic intrusive dyke, felsic
Lamprophyre dyke
Andesite flows
* ** * *1*.•—••y \\-7 J \ -.
\N... \ ••\ \
*V^^
\
\*\~^-
o^ ^ ^
"""""""^^^ V 2 ^
r ^v ^v. *- X^ ^ '.CD^ ''-t0.023/4.0 "~ *~ -~ ^^^V __
^--^ ^ 2 \
^0.003/3.0 N*N" X*N- ^N, ^^ \
X. ~ ^**V *
B.LOOS*'"--..
\ 6
5ft ion
40E
O O IO
To accompany a report by: J.L.TINDALE A ASSOCIATES INC.
ASQUITH RESOURCES INC.
MATONA MINE PROPERTYSHINING TREE GOLD AREA
Tyrrell Twp., Ontario
DETAIL GEOLOGY
Hare Creek Gold ZonePrepared by: K. W. J.
Drawn by : R. T. M.
Dolt: November 1 988
Scale: ( inch * 5ft.
Owg. No.
4tPHNEa4O9 63.5453 T YRRELL 250
o en oCO
5o4-
O
o 10 o inz o o
10oCM
o-V
ooo o in4- 4-o w
''-\ _. i Tr./2-O
~-~- \
2,3 . .j27.30 L Tr. sample .-,
0.068/4.0-^^
.028/5.O O.OS8/I.O
V—Elev. -10.^2'L— O.OOI/I.O 0.001/3.0 H
SYMBOLS
-——— Geologicol contact
—~~-i~—- Shearing
7p"~ Bedding , strike and dip
^ Survey point
~^ ~~ Fault /one
8
O.02/3.0 j Sample i l oz/ to i '
interval ; Au/width in ft.
GEOGICAL LEGEND
Quartz vein , crystalline
Siliceous lamprophyre with xenolith* of quartz - eye porphyry S black chert
Lamprophyre dyke
Quartz eye porphyry intrusive
Laminated silstones ft impure chert
Sulfide iron formation
Chert breccia in lamprophyre
Black chert , vitreous
Graphitic slates
Andesite, fine- grained
Elev. -5.08'L
Elev. -27.30'L
.-••••••...••' \....f O m ~' l
\
\
\ ;o
p
4O.OI6/3J
k*
^K0.001/3.O
0.021/4.0
* T
0.007/2.0
O.I79/2.O5.049/4.O
-2v-^"^*0.001/1.0
Elev.-17.87'L
— - — i - —. — —
O.OI8/2.5
.•.••••....L...--"'
Jo.ooi/i.o 0.494/1.00.136/2.0]
0.203/3.0
5ft lOtt
oinz o o
ro4*
M
O CM
•*-CM
Z O -*-
CM
O O-*
CM
Oen oCO
or- o(O
*o
z o o
10 To accompany a report by:
J.L.TINDALE b ASSOCIATES INC.
a
Shaft Elev. O.OO' L
ASQUITH RESOURCES INC.
MATONA MINE PROPERTYSHINING TREE GOLD AREA
Tyrrell Twp., Ontario
DETAIL GEOLOGY Matona Mine Property
Prepo'-d: K.W. J.
Drawn by -. R. T. M.
Oott: November 1988
Scale-, i inch - 5 ft
D w g. No.
63.5453 TYRRELL 260