oreco mines s energy corp. - ontario · 2017. 1. 17. · arthurian resources limited held the...

JAMES E. TILSLEY ft ASSOCIATES LTD.

4ineNE93S5 63.5143 SCADDING 010

ORECO MINES S ENERGY CORP.

SCADDING TOWNSHIP PROPERTIES

Sudbury Mining Division, Ontario

James E. Tilsley S Associates Ltd. Consulting Geologists and Engineers Aurora, Ontario, Canada L4G 3G8

Januar


41I10NE9365 63.5143 SCADDING

TABLE OF CONTENTS

SUMMARY AND CONCLUSIONS

INTRODUCTION

LOCATION AND ACCESS

CLIMATE

TOPOGRAPHY

LOCAL RESOURCES

PRO PERTY

LIST OF CLAIMS

SURFACE RIGHTS

HISTORY

GENERAL GEOLOGY

MINERALIZATION

PRODUCTION

RESERVES

EXPLORATION POTENTIAL

EXPLORATION PROGRAM

ESTIMATED EXPLORATION COSTS

CERTIFICATE

REFERENCES

Appendix I

Appendix II

1

2

3

4

4

5

6

6

7

8

10

14

20

20

20

22

26

Appendices

Details of claims

Location of diamond drill holes

010C

JAMES E. TILSLEY Bc ASSOCIATES LTD.

MAPS

Claims Location 1:31 680 Following pg 5

General Geology of 1:31 680 Following pg 9 Properties


SUMMARY AND CONCLUSIONS

Oreco Mines St Energy Corp. has optioned 23 mining claims

located in Scadding township, Sudbury Mining Division, Ontario.

The claims are in two groups. The larger group of 20 claims

lies on the eastern shore of Lake Wanapitei, more specifically

along Outlet Bay and Southeast Bay. The three-claim group lies

east of the Kukagami Lake Road, just south of the southern

extremity of the west arm of Ashigami Lake. Both groups adjoin

the Orofino Resources Limited property on which that company has

published reserves of 136 500 tons grading 0.21 ounces gold#ton.

The claims are underlain by metasedimentary rocks of

Huronian Age which have been cut by Middle Precambrian Nipissing

gabbro and related intrusive material. The youngest rocks of

the area are Late Precambrian olivine diabase dykes.

Although there are no known mineral deposits on the

properties, the claims cover sedimentary and igneous rocks which

host base and precious metal concentrations in the Scadding-

Davis-Rathbun township area. We consider the probability of

mineral deposits existing within the claims described to be high

enough to warrant careful exploration of the properties.

Exploration on the claims should include line cutting,

geophysical surveys, geochemical surveys, general and detailed

geological mapping, trenching, stripping, sampling, et cetera,

with an allowance for diamond drilling of targets lying under

overburden too deep or wet to be excavated to bed rock.

The cost of the recommended exploration program is

estimated to be S161 270.00.


INTRODUCTION

Oreco Mines S Energy Corp. has entered into an option

agreement covering two groups of mining claims (Wanapitei Group

- 20 claims: Ashigami Group - 3 claims) located in Scadding

township, Sudbury Mining Division, Ontario.

The properties adjoin claims held by Orofino Resources

Limited. The Scadding gold deposit lies within the Orofino

property. Published reserves are approximately 28 600 ounces of

gold in 136 500 tons of mineralized zone.

The Oreco Mines S Energy Corp. claims cover sedimentary and

intrusive rocks which host precious and base metal concent

rations in other parts of the area. Exploration for gold,

silver, platinum group metals, and base metals is recommended

within the properties. Exploration targets include breccia

zones such as host the gold mineralization at the Scadding Mine,

quartz-carbonate veins in both sedimentary and igneous rocks,

and copper-nickel concentrations with gold, silver, and platinum

group metals in Nipissing gabbronorite, similar to the Rathbun

Lake deposit.

The estimated cost of the proposed exploration program is

270.00.


LOCATION AND ACCESS

The property includes two groups of mining claims located

in Scadding township, Sudbury Mining Division, Ontario. The

larger group of 20 claims lies on the eastern shore of Lake

Wanapitei, specifically, along Outlet Bay and Southeast Bay.

Approximate co-ordinates: (Wanapitei Group)

46 0 41 1 30"N; 80 0 39' 00"W:

The three claim group lies east of the Kukagami Lake Road,

immediately south of the end of the southwest arm of Ashigami

Lake, in the unsubdivided portion of Scadding township but

adjoining Lot 5, Concession II.

Approximate co-ordinates: {Ashigami Group)

46 0 39' 00"N; 80 0 36' 00"W:

The claim groups can be reached from Sudbury Airport in

about one hour via Highway 17 East to the Kukagami Lake Road,

then eight miles north through Street and Scadding townships.

The Wanapitei claims can be reached via a local cottage

property access road that leads west from the Kukagami Lake road

in Lot 6, Concession III, past Bugg and Spar lakes for a

distance of approximately two miles to private cabins on the

south shore of Southeast Bay of Wanapitei Lake, within claim No.

S-943196 of the group.

The Ashigami Lake claims may be reached on foot

approximately one half mile east from the Kukagami Lake road in

the southern half of Lot 5, Concession II.


CLIMATE

The area has a continental climate typical of central

Canada. Precipitation totals approximately 34 inches (863mm)

per annum, relatively well spread throughout the year. Snow

accumulations of 700 to 1300mm are frequently observed in

average winters, with first significant falls in late October or

early November. Continuous cover can be expected from early

December until mid-April in most years.

Summer-time maximum temperatures may exceed 30 0 Celcius and

winter minimums in the range of -40 0 C are not uncommon in January

and February. Mean summer maximums are approximately 23 0 Celcius

and mean summer minimums about 12 0 C. Winter mean maximums are

in the range of -7 0 C and mean minimums -21 0 C.

TOPOGRAPHY

Lake Wanapitei has an elevation of 269m (882 1 ) above sea

level. Within Scadding Township the land rises to approximately

335m (1100 J ). In general, the surface is rolling, with

occasional abrupt hillocks of bedrock, especially along lake

shores where low cliffs are common. Relief is usually less than

30m (100'). There are some low-lying swampy areas but the

greater part of the land of the Township is relatively dry.

Drainage in the 20 claim group is west to Wanapitei Lake,

Wanapitei River, the French River and Georgian Bay. The north

ern part of the three claim group drains north to the western

4


arm of Ashigami Lake, then via the Sturgeon River to Lake

Nipissing. The southern part of the group drains to Timminsi

Creeks and, eventually, joins the Wanapitei drainage system.

LOCAL RESOURCES

Sudbury is a city with a population of approximately one

hundred and sixty thousand. There is a long history of mining

and smelting with a skilled work force in both mining and

related support functions. Men, equipment, supplies, and

services are all available locally.

Medical facilities are excellent, with several clinics and

hospitals in the city.

Rail, highway, and air transportation are excellent to

southern Ontario and points east and west of Sudbury.

The claims are forested with several varieties of pine,

spruce, balsam fir, cedar, and assorted deciduous species. Some

of the timber is merchantable but there have been no recent

lumbering or pulp wood operations.

Industrial power is now available within two miles of the

Wanapitei property at the Orofino Resources Limited mill site

which lies within one half mile of the Ashigami Lake claims.

Local transmission lines follow the Kukagami Lake road. Tele

phone communications, local and international, are possible from

homes and businesses in the area of the claims.

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ORECO MINES S ENERGY CORP.Scadding Township


CLAIMS LOCATION

Scale 1:20 000

MAP


PROPERTY

The properties consist of two groups of mining claims, the

larger including 20 claims along Southeast Bay and Outlet Bay of

Lake Wanapitei, and including the peninsula that separates the

two bays. The claims extend to, but do not include lands

beneath the waters of Lake Wanapitei, nor are any of the islands

in the lake open for staking. The twenty claims in the

Wanapitei Group require filing of 20 days work on or before July

23, 1987, the first anniversary of recording.

The three claim group also lies in the unsubdivided portion

of Scadding township. The surface and mining rights are owned

by the Crown. The claims in this group require 20 days of work

credits to be filed before March 25, 1987.

LIST OF CLAIMS

Wanapitei Group

S943192 to S943211 inclusive.

Ashigami Group

S865074 to S865076 inclusive


SURFACE RIGHTS

The claims cover Crown Lands with the exception of

approximately fifteen acres designated ?Plan M-623? and an

adjoining parcel AE.983 surrounding several cottages with

frontage on Southeast Bay. Use of surface rights on Crown

Lands is governed by the standard regulations. Use of surface

rights to the lands described in Plan M-970 must be negotiated

with the private owners.

There is also the standard 400 foot surface rights reserv

ation along the shores of Lake Wanapitei. Use of this land is

restricted except with prior permission from the Department of

Natural resources.


HISTORY

Gold was first reported from the Scadding township area in

the fall of 1891. (Ontario Bureau of Mines, 1892 p.237) The

discovery may have been made during surveying of the Scadding

Rathbun township line. The location given for the initial

discovery is not specific enough to be correlated with any of

the presently known prospects or deposits.

There is some evidence of stripping and trenching within

the properties but this work appears to date from about the turn

of the century since all trenches are slumped and overgrown by

vegetation.

The area was prospected for radioactive minerals during the

uranium rush in the 1950s following the discovery of the

uraniferous conglomerates at Elliot Lake. Subsequently the area

including both claim groups was covered by an airborne magnetic

and electromagnetic survey done by Kennco Explorations (Canada)

Ltd. in 1968. The Ashigami Group was included in the area

covered by an airborne magnetometer, electromagnetometer, and

radiometric survey done by Gulf Minerals Canada Ltd. in 1972.

The Ashigami claims were covered by reconnaissance magnetic

and VLF-EM surveys in 1984. This work indicated several areas

of anomalous magnetic responses and conductivity.

Arthurian Resources limited held the Wanapitei Group from

1982 to 1984. Magnetic and VLF-EM surveys were done on the

property. Line and station spacing were adequate for

8


reconnaissance of the claims and have indicated several contacts

and conductive structures (faults) which appear to warrant

additional investigation. Geochemical surveying in the claim

group south of Southeast Bay outlined several locations where

gold content of humus samples is at least twice apparent

background and have been interpreted (Meyer, 1984, Assessment

files, MND&M, Sudbury.) to indicate elevated gold content in

underlying, probably albitized, sediments in the same environ-i

ment as the Scadding Mine deposits.

Seven diamond drill holes were put down in the southeastern

corner of the Wanapitea Group in late 1984 (See Appendix II).

These holes intersected relatively widespread albitization of

basal Serpent Formation and Serpent - Espanola transition rocks.

There were no mineralized zones cut in the holes although Meyer

interprets the albitization and chloritization of the sediments

to indicate that processes similar to those that produced the

Scadding Mine deposits were active in this location.

The claims were optioned by Oreco Mines St Energy Corp. in

January of 1987.


GENERAL GEOLOGY

Reconnaissance geological mapping in the Sudbury area was

done as early as 1853 when Alexander Murray conducted river

and lakeshore traverses that included the Wanapitei River and

parts of the shoreline of Lake Wanapitei. Bell and Barlow

worked in the Sudbury Basin beginning in 1888 and included part

of the Wanapitei Lake area in their map published in 1891.

Collins worked to the south of Lake Wanapitei in 1912 and

reported his results in 1914. It was not until 1921, when

Quirke mapped Scadding township as part of his regional study,

that a geological compilation covering the claims that make up

the Oreco Mines S Energy Corp. groups was completed. Fairbairn

mapped Scadding township as part of his 1938 Ashigami Lake

project. Cooke et al., prepared the Falconbridge sheet in 1946

and revised Quirke?s 1922 map. Thomson mapped Scadding and

Maclennan townships during the 1956 to 1959 field seasons but

did not re-map those areas covered by Fairbairn in 1938.

Thomson reported his findings and presented a compilation in

1961 (ODM Geological Report No.2 and Map No. 2009). The most

recent study of the area is based on field work by Dressler and

assistants in 1977 and 1978 described in Ontario Geological

Survey Report 213.

The geology of the Wanapitei Lake area is summarized in the

following table from Dressler (1982) and applies to the portions

of Scadding township within and adjacent to the property.

10

JAMES E. TILSLEY A ASSOCIATES LTD.

TABLE OF LITHOLOGIC UNITS FOR THE LAKE WANAPPTEI AREA.

PHANEROZOIC CENOZOIC

QUATERNARYRECENT

Swamp, lake, and stream deposits.PLEISTOCENE

Glacial and glaciofluvial sand and gravel deposits.

UnconformityPRECAMBRIAN

LATE PRECAMBRIANMAFIC INTRUSIVE ROCKS

Olivine diabase.

Intrusive Contact MIDDLE PRECAMBRIAN

SUDBURY NICKEL IRRUPTIVESublayer, norite, transition zone norite, micropegmatite, granitic rode.

Intrusive ContactWHITEWATEROROUP

ONAPING FORMATIONTuff, quartzite breccia.

SUDBURYEVENT Explosive volcanism or meteorite impact; Sudbury-type brecciation.

NIPISSING INTRUSIVE ROCKSGabbro, granophyre, granitic dike rock, pegmatite, quartz-plagioclase

porphyry.

Intrusive Contact HURONIAN SUPERGROUP

COBALT GROUPLORRAIN FORMATION

Arkose, subarkose, subarkosic wacke, quartz wacke, arenite*.GOWGANDA FORMATION

Wacke, arkose, conglomerate.QUIRKE LAKE GROUP

SERPENT FORMATION

Arkose, arkosic wacke, calcareous arkose, minor conglomerate.ESPANOLA FORMATION

Calcareous siltstone, limestone, calcareous wacke.BRUCE FORMATION

Conglomerate, pebbly wacke, minor arkose, wacke.HOUGH LAKE GROUP

M1SSISSAGI FORMATION

Arkose, subarkose, arkosic wacke, subarkosic wacke, conglomerate, and silty wacke.

Unconformity EARLY PRECAMBRIAN

MAFIC INTRUSIVE ROCKSDiabase, glomeroporphyritic diabase, porphyritic diabase.

Intrusive Contact

11


FELSIC PLUTONIC ROCKSGranodiorite, diorite, migmatite.

Intrusive ContactMETAVOLCANICS AND METASEDIMENTS

METASEDIMENTSWacke, arkose, gneisses, ironstone, ferruginous chert

METAVOLCANICS

FELSIC METAVOCLANICS

MAFIC AND INTERMEDIATE METAVOLCANICS

Mafic and intermediate metavolcanics, amphibolite, dacite.

Scadding township lies just to the east of the eastern end

of the Sudbury Basin structure, the Wanapitei claim group being

approximately six miles east of the rim of the basin at the

village of Bolands Bay. The Sudbury Basin is generally thought

to have resulted from impact of an asteroid-sized body (l to 3km

in diameter) at about 1850Ma before present. The Wanapitei

structure, currently occupied by Lake Wanapitei is also believed

to be caused by an impact event at about 37Ma before present.

There is no evidence that either of these impact events

directly influenced mineralization within the claim groups under

consideration.

The area has been glaciated during Pleistocene time.

Deposits of till, outwash sands and gravels, and clay and silt

cover much of the bedrock inland from Lake Wanapitei. Depth of

overburden is generally less than 1.5m on higher ground but may

be considerably thicker in intervening till and glacial outwash-

filled swales and swampy areas. The last ice advance was from

the north with most striae indicating a direction five to ten

degrees east of true north.

12


Consolidated rocks of the area range in age from Early

Precambrian to Late Precambrian. The sedimentary rocks are

dominated by Huronian Supergroup clastic and carbonate

formations, and igneous rocks by Nipissing gabbro and related

phases.

The Huronian rocks mapped on the property include Espanola

Formation limestones and Serpent Formation arkosic sediments, of

the Quirke Lake Group and conglomerates, pebbly wacke, minor

arkoses and wackes of the Bruce Formation. Huronian sediments

are cut by gabbros assigned to the Nipissing intrusive suite. A

Late Precambrian olivine diabase dike is mapped in the northwest

part of the claim group.

The attitude of the sedimentary units in the Wanapitei

claims is variable, strikes are generally to the northeast and

dips range from 15 0 to 70 0N. An anticlinal axis extends into

the property along the portion of the Southeast Bay access road

that runs almost due north from the northeast corner of Lot 9,

Concession III.

The Bruce Formation rocks that are mapped in the three-

claim group are in fault contact with clastic sediments of the

Mississagi Formation of the Hough Lake Group along the eastern

limit of the block. The Mississagi Formation rocks strike

approximately east/west and dip steeply to the north. The Bruce

Formation rocks west of the faults appear to have similar

attitudes.

13


The contact relationships between the sedimentary rocks and

the intrusive gabbro are not well known. The Nipissing gabbro

is present as both a flat lying and nearly vertical dikes. The

olivine diabase body which is mapped where it passes through the

northwestern part of the property is a well defined, nearly-

vertical dike.

MINERALIZATION

Gold and base metal mineralization in the Scadding-Rathbun-

Davis township area is observed in three, probably-related

environments.

One type of mineralization appears to be related to

emplacement of quartz-carbonate veins and veinlets in fractures

in and adjacent to fault zones in both sedimentary and igneous

rocks of the property.

Gold is present in the native state, usually on the margins

of the veins and veinlets that we have inspected in the area.

Visible gold appears to be in relatively large grains of one to

thirty milligrams and to be randomly distributed in the quartz-

carbonate veins and veinlet systems. Assays of samples we have

taken from the the vein-type showings indicate that there is also

some fine gold that is not likely to be visible in hand specimen,

but the limited data that are available suggest the greater part

of the metal is present in relatively coarse grains.

Chloritization associated with the fault-controlled quartz-

14


carbonate vein systems may be even more pervasive than carbonate

addition. Both gabbros and sediments appear strongly chlorit-

ized in all locations where precious metal values are reported.

In some exposures of quartz-carbonate mineralization, original

rock forming minerals have been totally replaced by chlorite so

that identification of the host rock becomes difficult at the

hand specimen level.

The second type of mineralization is typified by the

auriferous zones of the Scadding Mine on the Orofino Resources

Limited property in Lots 5 and 6, Concession II, Scadding

township. These mineralized zones are described as ?breccia

pipes? which are characterized by strong chloritic alteration

which may make up 4(^ to 50* of the rock, with quartz in veins

and veinlets and as part of coarsely recrystallized quartz-

plagioclase groundmass. Minor carbonate, biotite, rounded

apatite, and detrital zircons are also present. The auriferous

breccias contain pyrite, chalcopyrite, pyrrhotite, arsenopyrite,

magnetite, galena, minor silver, and very low palladium.

(Martens et al., OGS Misc. Paper 91, 1979, pp 111-113.)

Not all quartz-carbonate vein systems or known breccia

pipes are metal-bearing. Neither is there an obvious

relationship between intensity of chloritization and base or

precious metal values.

It is postulated by Martins et al., (op. cit., 1979.) that

the base and precious metals are derived in part from the

Serpent Formation subgreywacke and siltstones with enrichment by

15


solutions originating in the Nipissing gabbro. This inter

pretation suggests that the areas of the property most

favourable for development of both vein-type and breccia

mineralization would lie near to, and within Serpent Formation

arkosic to silty sediments. The silt content of the sediments

is considered by Martins to be important as a metal source. The

lower energy environment of deposition characteristic of the

Espanola Formation is observed to be more conducive to fine

sediment deposition than the generally higher energy, near-shore

environment characteristic of the Serpent Formation arkosic

clastic sediments. Martins suggests that the best areas for

prospecting for the breccia type mineralization is near to the

Espanola Formation - Serpent Formation contact.

A third deposit type in the area contains copper-nickel,

gold, and platinum group metals mineralization. It is related

to the Wanapitei intrusion, a ring shaped, Nipissing gabbro

norite sheet centered on Portage Bay, Lake Wanapitei. The

deposit is described by Rowell and Edgar, 1986, (Econ. Geol.

Vol. 81, 1272-1277). This mineral occurrence is located about

four miles from the north boundary of the Wanapitei claim group

at the south end of Rathbun Lake, near the northern margin of

the intrusion as exposed in Rathbun township. The sulphide

mineralization is reported to be associated with extensive

fracturing of the gabbronorite and north-northwest trending

faulting. The mineralized zone strikes at 135 0 which is

16


perpendicular to the margin of the intrusive and dips at 60 0 to

the north. Massive sulphides were observed along a strike

length of 14m and varied in width from 0.3m to 0.6m.

Disseminated mineralization around the massive 'core 1 gave a

total mineralized width of about 3.0m

This mineralization is of interest in that it is inter

preted to have resulted from hydrothermal activity centered on

the fractured gabbronorite, and remarkable in that it is one of

the few known cases where platinum group metals are found in

this sort of mineralization environment.

The minerals identified in the study by Rowell and Edgar

include chalcopyrite and pyrite which make up 55% and 40% of the

total sulphide content of the zone. Present in 'accessory'

amounts are millerite, violarite, magnetite, goethite,

pyrrhotite, covelite, and molybdenite. Platinum group minerals

identified by these authors include merenskyite, kotulskite,

temagamite, michenerite, and rare sperrylite.

The grade of the sulphide zone is not properly established

by the sampling information available. Dressler, 1982, (OGS

Report 213, pp 100-101 - quoting Koulomazine, 1955, and Ogden,

1957) reports the massive sulphides returned values as follows:

Cu, 5.51 to ig.92%; Ag, 0.17 to 1.978 oz./ton; Ni, 0.11 to

2.86%; Pt, 0.088 to 1.08 oz./ton; Au, 0.002 to 0.36 oz./ton;

Pd, 0.17 to 0.98 oz. ton.

Dressler's sampling of the massive sulphides returned:

Cu, IQ.2%; Ag, 2.22 oz./ton; Ni, Q.14%; Pt, 0.056 oz./ton.

17


Disseminated mineralization (grab sample) from southwest of

the shaft returned: Cu, 1.3^; Ni, Q.29%; Pt, 0.07 oz./ton;

and Pd, 0.16 oz./ton. ( Dressler, 1982, op. cit. pp 101).

The origin of mineralization in Scadding, Rathbun and Davis

townships appears related more or less directly to emplacement

of the gabbronorite intrusive bodies. It is postulated by

Martins that metals were collected syngenetically in the silty

phases of the Serpent Formation sediments, and in the Serpent -

Espanola transition rocks. Further, he suggests that the metals

were remobilized by solutions generated or mobilized by the

gabbronorite intrusions, and concentrated locally in veins and

breccia pipes. He concedes that metal was also introduced

directly from the gabbronorite.

In any case, the gabbronorite intrusion appears to play an

important role in the three types of base and precious metal

mineralized zones described in the area of the claims. We have

observed gold-bearing quartz veins cutting chloritized gabbro

about four miles east of the Oreco Mines S Energy Corp. property

and interpret data from that location to suggest that the

mineralizing event is at least late stage Nipissing. The

mineralized breccia pipes on the adjoining Orofino Resources

Limited claims are described as 'Sudbury breccias' and it is

suggested by W. Meyer (personal communication 1987) that much of

the brecciation in the Scadding township area is related to the

Sudbury Event (meteor impact) dated at approximately 1850Ma.

18


The Nipissing intrusive is dated at about 2150Ma which suggests

that the mineralized breccias in Scadding township are more

likely related to activity during intrusion of the gabbronorite

and pre-date the Sudbury Event by a significant time. We

suggest that the Nipissing intrusive may have been emplaced at a

shallow depth in the crust, and that the breccia pipes in

Huronian sediments are related to gas brecciation which is not

uncommonly observed to accompany shallow level intrusion,

particularly those emplaced into wet sediments, such as could be

expected in this location. Further, it seems reasonable to

assume that those (gas) breccias related to the Sudbury Event

are likely to be unmineralized, given that the time of develop

ment would be measured in minutes rather than millenia.

The exploration problem would then lie in differentiating

between fluidization breccias caused by intrusion of the gabbro

norite and those that were caused by explosive degassing related

to the Sudbury impact event. Since there is no evidence that

rocks of Sudbury Nickle Irruptive affinity are present in the

area of the claim groups, it can be assumed that there have been

no widespread mineralization events since emplacement of the

Nipissing gabbronorite. Late Precambrian olivine diabase dikes

are present in the area and within the claim groups. However,

there is no evidence that these dikes have applied sufficient

energy to the environment to develop notable concentrations of

metals in Scadding township.

19


PRODUCTION

There has been no recorded production of metals from the

property.

RESERVES

There are no known mineral reserves on the property.

EXPLORATION POTENTIAL

Although there are no known mineral deposits within the

Oreco Mines Se Energy claims, the properties cover rocks that

host at least three types of metal deposits in the Scadding-

Rathbun-Davis townships area.

1. Quartz-carbonate veins localized in fault zones cutting

the Huronian sediments and the Nipissing mafic intrusive rocks

are known to carry base metals with gold and silver.

2. Breccia pipes in sediments of the Quirke Lake Group,

(Serpent and Espanola Formations) have been explored on the

Orofino Resources Limited property that adjoins both of the

Oreco Mines Si Energy Corp. claim groups. Published reserves on

the Orofino ground are 136 500 tons containing 28 665 ounces of

gold (Scadding Mine).

3. Massive and disseminated sulphides containing copper,

nickel, gold, silver, and platinum group metals have been

deposited in an apparently hydrothermal system developed along a

fault#fracture zone at the edge of the Wanapitei gabbronorite

20


intrusive in Rathbun township (Rathbun township type).

All three types of mineralized zones are possible within

the Oreco Mines S Energy Corp. Scadding township properties.

Although there is no mention in the literature of such

mineralization, it is also possible that there may be base and

precious metal bearing scarn deposits developed at the contact

of the Nipissing intrusive with Espanola Formation limestones

and Espanola - Serpent transition rocks. Cumulate type mineral

concentrations may have developed at the bottom of parts of the

Nipissing gabbronorite sheet. There is some geochemical

evidence of Cu, Ni, Ag, Au, Pd, and Pt, enrichment toward the

base of the gabbronorite sheet (Dressler, 1982, op. cit.) While

this possibility should be borne in mind during interpretation

of results of geophysical and geochemical surveys, and any

sulphide concentrations within or adjacent to the Nipissing

intrusive should be checked for gold and platinum group metals,

there is little evidence to suggest that this type of mineral

ization is a prime exploration target on the properties.

Quartz-carbonate veins are possible throughout all of the

sedimentary and intrusive rocks of the properties. Breccia

bodies similar to those on the Orofino Resources Limited

property may, in our opinion, be hosted by any rocks older than

the Nipissing intrusives. It is suggested by Martins that the

most favorable environment for breccia type mineralization would

be near to the Espanola Formation - Serpent Formation transition

21


along the southern boundary of the Wanapitei claim group.

Results of exploration on the three claims south of Southeast

Bay filed with the Mining Recorder in Sudbury (Meyer, 1984,

Assessment files, MND&M, Sudbury) indicate that there is some

breccia and albite alteration in this area, and that further,

more detailed, exploration is warranted. We suggest, however,

that exploration for breccia type deposits not be limited to

these claims.

The area most favourable for development of the Rathbun

township type of hydrothermal mineralization within the claims

under consideration is along the eastern shore of Southeast Bay,

in the Wanapitei claim block.

EXPLORATION PROGRAM

Exploration for vein type mineralization in both the

sedimentary and igneous rocks of the properties can use electro

magnetic and magnetic geophysical techniques for definition of

structural features likely to host this sort of deposit.

Geochemical surveying along such structural features has been

proven to give information which assists in location of base and

precious metal-bearing zones. Stripping, mapping and sampling

of targets indicated by results of geophysical and geochemical

work is a necessary further step in the evaluation of any

indicated or suspected mineralized zone.

The breccia type mineralized zones have relatively smalX

22

JAMES E. TILSLEY A ASSOCIATES LTD.

surface areas. Magnetic expression can be either positive or

negative, and is restricted to the zone of alteration that

is associated with base and precious metal values. In general,

line spacing of 50 to 100 meters with stations not more than 10

meters apart is appropriate in the areas underlain by sediments.

However, the density of magnetic determinations in areas where

breccia pipes are thought to be possible must be high enough to

ensure that a relatively detailed sampling of the magnetic

features of the zone are well documented and limits can be

defined accurately. This may require stations established at 2

to 5 meter intervals on lines 10 to 15 meters apart.

The breccia zones themselves are not likely to be indicated

directly by electromagnetic surveying, but zones of fracturing

and faulting which might exert some control on breccia formation

may be outlined by such surveys.

Geochemical surveying will indicate the presence of base

and precious metals through overburden cover that is not of

excessive depth. We have found collection of forest mull (or

?humus?) to be the most effective geochemical survey sampling

technique in the Scadding township area, since this material

will indicate the chemistry of the soils and rocks penetrated by

the roots of the trees and shrubs from which it is derived.

This gives a greater depth of effective sampling than can be

expected when inorganic material is collected from the uppermost

soil horizons developed on transported overburden such as covers

most of the properties. Normally humus samples are taken on a

23


relatively wide spacing since there tends to be a dispersion and

mixing of leaves, needles and bark fragments from individual

trees or groups of trees growing on mineralized ground with

similar material from trees not in contact with mineralized bed

rock. This results in broad, low amplitude, metal anomalies

from restricted source areas. Reconnaissance sampling is

recommended for those parts of thfe property which have not been

covered, and more closely spaced sampling in the area of known

precious metal anomalies and any base or precious metal

anomalies indicated by results of the reconnaissance sampling.

The spacing for reconnaissance sampling should be in the order

of 30m to 50m along lines not more than 100m apart. Detailed

sampling would have samples on not more than a 40m square grid,

with 20m square grid density in selected areas.

The humus samples respond well to analysis by neutron

activation techniques and are particularly suitable for deter

mination of gold content in the parts per billion range. We

have found that other elements are often useful indicators of

mineralization and usually opt for the total 16 element package

(Au, Sb, As, Ba, Br, Gr, Co, Fe, Mo, Se, Ag, Ta, Th, W, U, and

Zn) at a slight additional analysis charge. In the Scadding

township area, copper and nickel analyses may prove useful in

evaluating certain environments of mineralization.

Interpretation of geological and geochemical results with

reference to information collected during geological mapping of

24


the survey area should be followed by trenching, stripping,

washing, geological mapping, sampling and assaying, as required

and possible under overburden and drainage conditions existing

in those areas where data indicate the possibility of mineral

ized bodies.

Rathbun Lake type deposits appear most likely to be

developed in the claims along the contact of the gabbronorite

that parallels the east shore of Southeast Bay.

Since this type of mineralization is localized by faulting

and fracturing in the gabbronorite and likely to contain some

pyrrhotite and possibly magnetite, both magnetic and electro

magnetic techniques are appropriate. The strike length of this

type of mineralization can be expected to be in the order of 15m

to 45m. Therefore, the control grid line spacing for both mag

netic and electromagnetic surveying should be adequate to cut

any zone of these dimensions on at least one line, and station

interval should be close enough to detect the magnetic response

from a body of these dimensions.

The exploration program should include the activities

discussed above concentrated in areas of detailed investigation

selected with reference to results of existing reconnaissance

geophysical and geochemical surveys.

25


ESTIMATED EXPLORATION COSTS

The cost of the recommended exploration work is estimated

as follows:

Lines 64km profiles at 3230 14 720.00 6.0km base line at 5 325 l 950.00

Geophysical surveys; total magnetic 27 360.00 field, magnetic gradient, VLF-EM 2TX, 3 parameters 7200 sta. at 33.80

Geochemical surveys; humus sampling, 20 400.00 16 element analyses, 1200 stations at 317.00

Geological mapping; 64km at 3200 12 800.00

Trenching 10 000.00

Sampling 5 000.00

Diamond drilling (allowance) 20 000.00

Assaying 4 000.00

Supervision 5 200.00

Consulting, reporting 5 500.00

Drafting, secretarial, printing, 3 800.00 binding, et cetera

Communications, courier 900.00

Equipment allocations (pumps, 2 850.00 generators, hose, camp, et cetera).

Vehicles (incl. fuel, insurance, 5 400.00 et cetera)

Boat, motor, trailer (3 months) 2 490.00

Travel, room S board 8 900.00

Continency 10 000.00

TOTAL 3161 270.00

26


CERTIFICATE

I, James E. Tilsley, of the town of Aurora, Province of

Ontario, hereby certify:

1. I am a Consulting Geologist and reside at 5 Steeplechase Avenue, Aurora, Ontario.

2. I am a graduate of Acadia University, 1959, B.A., Geology.

3. I am a member of the Association of Professional Engineers of Ontario, The Association of Professional Engineers of Manitoba, The Association of Professional Engineers of Nova Scotia, Chartered Engineers (Great Britian), and designated Consulting Engineer, Ontario Association of Professional Engineers, 1975.

4. I have been employed as a geologist since graduation, with consulting groups since 1964 and in private practice since 1980.

5. This report is based on study of records relating to the property as available from the assessment files of the Ministry of Natural Resources, province of Ontario, reports of the Geological Survey of Canada, maps and reports published by the Ontario Bureau of Mines, the Ontario Department of Mines, and the Ontario Geological Survey, current technical literature, review of activities on the claims during the past five years, observations made while visiting the area during the past two years in the course of supervising an explor ation program in the northeastern part of Scadding township. The claims discussed have not been visited specifically in regard to preparation of this report due to winter conditions and snow cover.

6. I have no interest, direct or indirect, in the proper ties or securities of Oreco Mines S Energy Corp.,or any affiliates, nor do I expect to re&ajj/e any such interest,

Dated at Aurora, Ontario this 1987.


REFERENCES

Dressler, Burkhard O.1982: Geology of the Wanapitei Lake Area, District of Sudbury; Ontario geological Survey, Report 213, 131p. Accompanied by Maps 2450, 2451, scale 1:31 680 ( l inch to 1/2 mile) .

Fairbairn, H.W.1939: Geology of the Ashigami Lake Area, Ontario Department of Mines, Volume 48, 1939, Accompanied by Map 48m (Ashigami Lake Area)

Martins, J.M., et al1979: McLean-Watt Gold Property; in Annual Report of the Regional and Resident Geologists, 1979, edited by C.R. Kustra, Ontario Geological Survey, Miscellaneous Paper 91, 143 p.

Meyer, W.,1984: Report on an Exploration Program for Gold on the Company's Scadding Township Property, Sudbury Mining Division, Ontario for Authurian Resources Limited Ministry of Northern Development and Mines, Assessment Files, Sudbury, Ontario, pp 19.

Pye, E.G., et al, (Editors)1984: The Geology and Ore Deposits of the Sudbury Structure, Ontario Geological Survey, Special Volume l, 603 p. Accompanied by Map 2491, at a scale of 1:50 000, Map NL-16/17-AM Sudbury, at a scale of 1:1 000 000, and 3 charts.

Slaght, A.1894: Fourth Report of the Inspector of Mines; OntarioBureau of Mines, volume 4, 1894.1896: Fifth Report of the Bureau of Mines; 1895, p.56.

Thompson, J.E.1961: Maclennan and Scadding Townships; Ontario Department of Mines, Geological Report 2, 34p. Accompanied by Map 2009, scale l inch to 1/2 mile.

JAMES E. TILSLEY de ASSOCIATES LTD.

Appendix I

Details of claims


Abstracts

Ashigami Lake Claim Group

447194 ^^ —— TI—-.W--"-EDWARD JEROME C. 32301 4150* March 25,

S. 865074 -

1986AMICU MTI utm itmt M fiumt r.t.

A|L15 Clairview, P.O. Box 473 - - j ^al Caron, Ontario 4ar. 16/86 e 9:00a.m. Ix

orrtcc uci CULT ticoiiiB M""ef "*c""10" er et*'"

?;lii!

SDATC

Apr. 2 8/8 6

B*TS•O*IC

'

SCADDING TWP. (G. 3056)

Transfers all pj^tjOrest to P.A.R^-rBcown Licen

*

) MOUND Mi. LMOS M0 HNtM. RVCO.

ns.no.

S. 865074

ce*————————————— THIS iifetratt it a eepy aflhe entries in tRa — — ———————————— , Record Book and is not to be considered K

C. 29927. assurance of the validity of the claim. {S. 865074)

/tea29J*bJz^-^J/

^3jJ*4wiNiNG RECORDERSUDBURY MINING DIVISION ^ '

•-.v.:..;••---"^..,

•ICIlfT NO.

4532^

AUDIT NUMBER

447195Ministry 01 Northern Oavetop CUUMNO

S.fi65075

EDWARD JEROME March 25. 1986

Clairview, P.O. Box 473 Val Caron, Ontario Mar.16/86 3 10:50a.m.

400 foot HJffACt mOHTB RESERVATION MOUND AU. UKES AND WVERSJMND AND OMVEL (CURVED. PEAT RESERVED

Apr.28/86 Transfers all intere . Brown Licence!This Abstract isParnrrt Rnnl/ n nC.29927. (S.865074)

AUCII HUMIC!

447196 md Mines i ICIWMIW. o~*o t Th* Mining Act P. 865076

KCOIOIB 1* THt MM Of ^ LICK C l MO. KCIIM NO. BITI IICOIBIB

EDWARD JEROME C. 32301 4150 March 25, 1986• DOI^J BATS AMB Tin I Of STAIIN* f.T.

^15 Clairview, P.O. Box 473 ' , J Val Caron, Ontario * *ar. 16/86 @ 12:30p.m. |x

"i

li

lo!l

orric. usi ONLY .^Jit. ML*NCt B"t"lrl10" or eul"

BATI

Apr. 28/86

DATS•otic


RESERVATIONS — 400 fOOT SUWACt mOHTt BE8MVATKJN ABOUND AU LAKES AND MVEflt •ANDANOIMAVELICSePIVEO.KATKKflVEO. ~* "** "™

FILE NO

S. 865074

transfers all interest to P. A. R. Brown Licence^.

-•29927. This Ahstract is a coov of the entries in the (S. 865074)Record Book and is not to be considered as assurance of the validity ot the claim.

/JEC29J|8kvXZ^^--*-^-*— ~S

sffir?iilBIWWI*WK)RnEB ^ ' j

•tctir: as.

532^

'

JAMES E. TILSLEY St ASSOCIATES LTD.

Abstracts

Wanapitei Claim Group

JlJlTrxft* (W) Northern Oevetopmem -* ;

447681 S; andMines ! TH. iumn, Aet jCUUMMO. . . .

S 94*^109 tCOIDED IN INI NIK or UCCHCC HO. *[CIIM MO. OATI IICOKCI

EDWARD A. JEROME C. 32301 5391 July 28. 1986AOD*II* ftATI AIIO Tint Of fTAIIIIt f,I.

A^5 Clairview, P.O. Box 473, Val Caron, Ontario July 21/86 e 6:00a.m.j POM 3AO i x

orricc u.i OMLT .tcSISio "1J"" 0"e"IMIOM or ct*'"

a

I!w"

Sf H

H i!

D1TI OKIE

SCADDING TWP. (G. 3056

^.

This Abstract is a copy of the entries in theRecord Book and is not to De considered as assurance of the validity of the claim.

)

1 AHOUNO AU. LAKES AND MVEI*.

fi Q4^1

OEC2t)19o5^

/L/^LtJ\TUMtNfi jtrT"-*--* i^

SI!D^*" M^ING flivtstoM^^n-T '

RftNCCIPT MO.

'

'- i

A A-i-tr\r\ fa?) NofUiern Devekxxnont "" W ..XiS^Btfe

447700 S --l*- U vi^lSIM!• ICOUIO IN 1MI HAM! or IICIXCI HO. UlCIIPt HO. Mtl MCM

REGINALD J. CHARRON i:. 29749 5391 July'AOOtltt OATf M* 1

^^ z Drive, Hanmer, Ontario POM 1YO 3\A.y .

orr,ci u.i ONLY ..Jilir. Ml"el OIlct""0" " e"'" , i -r v

a * fcl2*"o uliO ft-

fi

OUTI

'

'

DATSVOPK

SCADDING TWP. ;{G.

' •.•-'Zii'-f'i.'.-.•^^••2-

iî^^"0-Hi^B. 943211

2Jsf 1986MS *r muDM f.T.

.23/86^8 1: 10p.m. x

jS?^-t ^t . " L , -•"'1 * ^'-•C-^"*"rJ-i '-'1.;* "

RESERVATXJNS - WO TOOT tUWACB MOOTS IBUBKIIHI X*MII til WKES AND NVEttS •AND ANO OKAVB. MESBMDinwrMSBWB.

Including Land Under Water

..-;..-.- v...c'J-V-^'w ntiNO.

^" S. 94 3208^ -' - -' ' "" -' "

fills Abstract is a copy ot the entries m tne Record Book and is not to be considered as c, xratctlrarjra nf tha uiliriity nl thf claim. ' '

^ i gxr, ;;fi^-; . ' -" ^ *' ' fc.

/l^Lu^L^y ; ; vv: -^\I~?S - ..'i. -^ . - ..,:

S .,~ - . , - ' -' - V -- - i. 'KECORDtR '" " 0 " J-' r " -r f v . ^ ' ,.

ÎI'IHMV.'Y MIHINf! niVISION ' 1 "- ~

•'•-.•-'. V\*;;': ' t-;--'

..' '"''V' -" : :*.-"V?: •':'i'i ' " ' ' ""

-' : ••• : "' : ' V' :^T

"\. - •-.-••••:- ••'-':

- . . '- - - r . t '.

...; .^. . ." --v .

;- .; -' : : --'" -.--' "X-

•-"' .-'' V-T^.-''": " " '-V

"- - - ". ' - ' j - ".- ""'^^^^''jl"

-••C^^T^;^.; -

. -îSi^'^S

-•-s^^^Sl

. ..^tjyjj^Vl^^Jj*" ."-*?stejs

!W-- -W^fl^r^lAaJlgw^

^S^-,^':"' ' .

(^K^f-SjB?*'r ' '

'^^f^V

RICIIPT 10.

V

WOIMOI

i .i

447682 S -a—— } Th. B1.,.. ^ |EDWARD A. JEROME C. 32301

AfrPHtJ

ft

| H

liH

S. 943193•CCtlFT IO. PATI IICOIII*

5391 July 28, 1986M PAH AN* nmt OF (TAirnc r.t.

15 C lairview, P.O. Box 473, Val Caron, Ontario July 21/86 6 9i35a.ro. 1 POM 3AO |x

ornci u.i ONLT n 'inu **""" B"e""10" " c"'"


RESERVATIONS — 400 FOOT SURFACE MOHTS RESERVATION AftOUM) ALL LAKES ANO MVCRS. SAND ANO OfUVEL KCERVEO. FfAT MeSCMVCO.

OATl Dillmont

FILE NO.

S. 943188

Tfiis Abstract is a copy of the entries in thefarnfi) f^ont anri k not to hfi considered 8Sassurance of the validity oi the claim.

yotugyj&y/'"/X*NB*I -^ ^7 i* — \ .f^*

yF^^ MININGFRjn^*?flfi * *!Ml* \^ r^^^

SUDBURY MJNING DlVISIOf an — '

'

-. ' . '.^- .. -.

;

ttCIIPI HO.

- ;* : .

447683 2s -^ """"lIICOIOIO IN THE Hunt Of L ICCNCI "0.

EDWARD A. JEROME C. 32301

Th* Mining Act | S. 94 3194•CCIIM HO. till IICOIOIO

5391 Julv 28. 19861001(11 (ATI 1*0 tlDI OF milH* f.T.

9-5 Clairview, P.O. Box 473, Val Caron, Ontario July 21/86 8 ll:15a.m.j POM 3AO 1 x

ornci u., ONLY ..f*!',,, """" e"C""tO" Or S"'"

fi5 rt **

s*so

i!Dirt 5",*,


RESERVATIONS — WO FOOT SURFACE MOOTS RESERVATION AROUND AU UKES AND MVERS •AND AND GRAVEL RESERVED. KAT RESERVED.

FILE NO.

S. 9431

This Abstract is a copy of the entries in the Record Book and is not to be considered asassurance of the validity ot the claim.

/f^.'^T^/^Na —— "SUDBURY MIMING DIVISIUN ^ '

R8ItCIIM XO.

J

M M -*rx rt M lv J N^?™0ovotopment fl/l/Rxfl. Viix and Mines*T H 1 D O H OnUrio


Th.ml,Aet ^943195•tCIIPT MO. OATI IICOOIB

5391 July 28, 1986ODIICf* ' (ATI AND TIHC Of ITltlH* r.t,

^fc.5 Clairview, P.O. Box 473, Val Caron, Ontario July 21/86 @ 12:55p.ml POM 3AO (x

orr*. u.i ONLY .leSI.t* """" B""""0" or c"1"

• M t*

S35"t'

ifH

BtTI OATS•O UK


RESERVATIONS — OO *OOT SURFACE RIQHTS RESERVA1K9N AROUND ALL LAKES AND MVERS. •AND AND QRAVEL RESERVED. PEAT WSERVEO.

f ILE NO.

S.Q431

aa^fc*

This Abstract is a copy of the entries in the Record Book and is not tn he considered isassurance of the validity of the claim.

UtU 2 y Bdb

^/^^siiiJ&ijflWiaiMJUjrwt!?H^RDcn - '

'

/" : ."-' ;v-'-

. ,'* Cv.'.V * -

: ; v--,;'-.,..;. . ;

^ r: :\' . .

^ -

••^'M^-- - -- ~ : - - '

?8• IC[IPT HO.

MO (WO)

447685

r

*

9

9

*

9

tr^n\ " 'iflisiry OiIWJ Northern Development}*ZS end MinesOnlvto


j ICUUUNO.

l Th. Mining Act | S. 94 31 96• ICIIH HO. BAU lICOIBCt

5391 July 28, 1986ADDIIII DAT! (NO TIMI OF IIAIIHS

As Clairview, P.O. Box 473, Val Caron, Ontario July 21/86 6 2:30p.m. POM 3AO

• a 1 1S*l'

il!

omcc on ONLY KCOIDIO IM-*"ct

-

OATt OATS • OIIK

OUOIH ON OF CLAIM

P.T.


RESERVATIONS — 400 FOOT SURFACE RIGHTS RESERVATION AROUND AU LAKES ANO RNERS. SAND ANO ORAVEL RESERVED FEAT RESERVED.

Excl . Road

FILE NO.

S. 9431

— ,———— - ———————— Tiiia Aliilrzil is i copy 01 me eninea in me ———————————————

Record Book and is not to be considered as assurance of the validity of the claim.

DEC 9, 9 19bbJ ' ^

^^^^J^ . *' ACTING MINING RECORDER

'

38RICtlPt MO.

447686 S zzzzr~*™ j Th. *Mn9 Ae! 1^3197EDWARD A. JEROME C. 32301 5391 Julv 28. 1986

1BBI1M D*t[ AND TIKI OF tTAKIH* P.T.

As Clairview, P.O. Box 473, Val Caron, Ontario July 21/86 @ 4:05p.m. POM 3AO x

giH O

s 5

hf!

orrtct un ONLY nicolite •*1J"CI

B*T( Bin• OIK

OISOIPTION Of CLAIII


RESERVATIONS — *0 FOOT (INFACE MOHTS HESEHVATION AROUND AU. LAKE* AND NVEW. SAND AND (MAVEl. MSEHVEO. PEAT MESEMVED.

Excl. Road

FILE NO

S.94318fi

Hi Is nus[fac( is a copy 01 me enines m me Record Book and is not to be considered as assurance of the validity of the claim.

yfipH o Q ^K)y^'Cxu^^.C/'

^fciNWSa MINING RECORDER

SUDBURY MIKING DIVISION 1 '

'

IICtlPT DO.

447687 S2 -ndMln"EDWARD A. JEROME

UCINCC HO.

C. 32301

The Mining Aet S. 943198menu no. **il ticooDC*

5391 Julv 28, 1986ASOttfS (ATI AND lint Or (TAimc r.T.

Al5 Clairview, P.O. Box 473, Val Caron, Ontario July 22/86 8 8: 05a.m. POM 3AO x

P Ift?hli

ornci u*i ONLY

DATt BAYS•ODK

BAT*licensee

lALAMCC Ot'CHH ON OF CLAIM


RESERVATIONS — 400 FOOT •UOFACE MOHTS MESEHVATION AROUND AU LAKES AND WVEHS. CAND AND OHAVCI. MESEPIVEO. PEAT WS0IVED.

Excl. Road

FUND.

R. 9431

*-

^_

This Abstract is a copy of the entries in the Recoffl Book and is not to bo consisted as ———————————— : —assurance of the validity of the claim.

vy^Kclll^^MrSittJG MINING RECORDER

SUDBURY MINING DIVISION _ ' \

R fiicccirt no.

(S) nslaDevctop(nent i "— *•miOOO onuno ; Th* Mining Act S. 943199•ICOiBIB IN INC BtIC OF LICtNCI NO. ItCflPI 10. Dill IICOlOI*

EDWARD A. JEROME C. 32301 5391 Julv 28. 1986*P0K

31

mm

\\

li

:s

II Pitt AND TIME OF miINt P.I.

|b Clairview, P.O. Box 473, Val Caron, Ontario July 22/86 @ 9:35a.m.| POM 3AO Ix

OFFICC U*E ONLY KCOIOIO "LAHCt

-

out OAT I• OIK

DESCRIPTION OF CLAIM


RESERVATIONS — 400 FOOT SURFACE RIGHTS RESERVATION AROUND AU. LAKES AND NVERS. SAND AND GRAVEL RESERVED. PEAT RESERVED.

FILE NO.

S.9431J

————— : ———————— i Tills Abstract is e copy or me eninei m me —————————————————— Record Book and is not to be considered as assurance of the validity of the claim.

/OEQ 2 9/193&Vy/^X-4-tft-^,^/ ^^

' ASBSFMINING RECORDER SUOBURY MINING DIVISION ' J

-

J8RKI1PT MO.

•^ ^T 1 J ^? ^? Ontario


i Th* Mining Act S. 943200IfCIIPT MO, B*TC IHOICC*

5391 Julv 28. 1986traccu DAU AH* tint or ntuic T. t.

^5 Clairview, P.O. Box 473, Val Caron, Ontario July 22/86 @ ll:15a.mL POM 3AO Ix

emo o.i ONLY .icJJJiD ""*" D"""no" or cu""

5!Hlito

iD.tl DATS

VDMK


RESERVATIONS — 400 TOOT tORFACt BKJHTS WStdVATKJd ADOW0 AU LAKES AND NVEMS. SAMO AND OMVEL MEICMVED. KAT HESBMEO.

FLCNO

S. 9431

^^^This Abstract is a copy of the entries in the

assurance of the validity of the claim.

, /j^s^y*X ACT,i|M8GMHW

SUDBURY MINING

1G RECORDERDIVISION — '

- . " '

88• ICtlPT NO.

447690 On^nB "^M"** ( TM M |BJB9 A^ | s^ 943201

ntcoitio m INI Nine or

EDWARD A. JEROMEUCCBCC NO. MCflM HO. (ATI MCOHDCD

C. 32301 5391 Julv 28. 1986tDDKII Mil AND Tin t Or HAH** F.T.

^p.5 Clairview, P.O. Box 473, Val Caron, Ontario July 22/86 6 12:50p.mL POM 3AO Ix

• a

S 5g" l\s!!

OPTIC* un ONLY

PATt •OIK

itconi*

-

• •i * j* r f DCSCIIPTION Of CLAIM


RESERVATIONS — 400 FOOT WRFACC RWHTf RESERVATION AROUND AU LAKES AND RIVERS •AND AND ORAVEL RESERVED. PEAT RESERVED.

FILE NO.

S.Q431RR

^.Th;s Abstract is a copy of the entries in the Deport! Doah and 'a not to bo considered n —————————————assurance oi the validity of the claim.

fJFC f) 9 IQrfhWM" ft ^ tv^J+J

ff S~}Mf* If

\^iin *^"^

^U&BOfiV MNING- JHVtSWtKenrr-

'

.

•ICEIPT *0.

A A 7 R Q l S) rS***^*t *t 1 D 3 J. Onuno

MCOIBCB in 1MI MAIU OF LICIIICt NO.


It l ~" fcLAIUNO

tTh* Mining Act | S. 943202• ICtlFT HO. OAtt HtCOMIS

5391 July 28, 1986ABOICU I*T[ AN* Tine OF STAIIIIC F.T.

aflkS Clairview, P.O. Box 473, Val Caron, Ontario July 22/86 g 2:35p.m. w POM 3AO x

OFF.C. U.( ONLY *Kollu """" 0"M"110" Of SU'"

|

B• :B*Tt DtTS


RESERVATIONS — 400 FOOT SURFACE RIOHTS RESERVATION AROUND ALL LAKES ANO RIVERS •AND AND GRAVEL RESERVED. FEAT RESERVED.

FILE NO.

S. 9431

^^

This Abstract is a copy of the entries in the

assurance of the validity of tho claim.

y3EC^91^

/^^^^ \suD^u/ii nViiiii' tiiVISRW-' rtUcr1 _ *

B8• tCIIFT HO.

447692 S?Cnlano

Nor ihern Development andMmes i

Th* Mining ActCLAIM NO.

S.943203

EDWARD A. JEROMELICtttCt HO.

C. 32301 5391•ATI *ice*oio

Julv 28, 1986•ATI AMB TIM! Of

Clairview, P.O. Box 473, Val Caron, OntarioPOM 3AO

July 22/86 e 4:15p.m.

SSl*

IfSO

l

erncc usi ONLYOCfCfllrllON OF CLAIM

SCADDING TWP. ( G.3056)

RESERVATIONS *M FOOT SURFACE mOHTB FXSCKVATION ABOUND AU. tAKE* AND MVENS IVR FCS6F1VED- FtAT MC4EAVED. ANDANOOFlAV


FM.ENO

S.943188eatsWORK

ThTs"Abstract is a copy ot the entries in the,Record BOOK ana is not to be considered as assurance of the validity of the claim.

wo (S vat

StCOP!SUDBURY MINING DIVISION

447693 *vf^ l Northern OovQIOpfTlGnl CUUM NOjurto andMmes ? Th, Mlnirlg Ae| S. 943204

•ICOftttt IN 1MC H*MC OF

EDWARD A. JEROME

LICtNCC BO. UlCtiri BO. DATS HCCOMBfP

C. 32301 5391 July 28, 1986•OBDIU OATI AND Tt MI Of HAH** f.T.

3|fc Clairview, P.O. Box 473, Val Caron, Ontario July 23/86 @ 8: 00a.ro. ^ POM 3AO x

5;!* lin

H

orrics uic ONLY

BITE •o*K

•ATI mCOIBCD

MIA.ICI BltCtlFTIOH Of CIAIH


RESERVATIONS — OO FOOT SURFACE RIGHTS RESERVATION AROUND AU LAKE* AND MVBB (AND AND GftAVEi. RESERVED. PEAT RUERVED

FILE NO.

S. 943188

(PIS Abstract is a copy of the entries in the Record Book and is not to be considered isassuranrp nf the validity nf thfl rlaim

.J9

/(^LjS*^/^MMING

SUDBURY MIN1NR nfviMjP^DSR ' f

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ttctin io.

447694 oniwo "ndMine* Th* Mining Act S. 943205

EDWARD A. JEROMELiemct no. nccfirt no. o*it nicolet*

C. 32301 5391 July 28, 1986APVmi OATC AND TIMC OF fllllHC f.T.

AL5 Clairview, P.O. Box 473, Val Caron, Ontario July 23/86 @ 9:35a.m. ^ POM 3AO x

5 11 w

xS

H

liU

orricc u*i ONLY

DtTt • ATIwont

BATf•ICOIDtD

•AiANct B""IMION or euw


RESERVATIONS — *0 fOOT SURFACE MIOKT8 MEtCHVATKM ABOUND AU LAKES AND WVEBi. •AND AND GRAVEL HESEMVED. KAT mtBNlO.

Including Land Under Hater

FILE NO

S. 9431

This Abstrsct is a copy of the entries in thenfiCOFu buuk AMU o iK*l lu ve vOliiiU6iiJ oAassurance of the validity of the claim.

DEC 2 9 ttfe

^LL^[J5JWWJRY MINING DIVISION ' |

ACT..,v3 i.iiHiiMbi hcCviaDEF)

t

B8ItCtlPT 10.

. . — -^-. 1 VV l Northern Development ••" * - ' OMUHO ————————————

447695 S^"1^ 1th. Mining Ae, S. 943206

EDWARD A. JEROME C. 32301• ECIirt HO. VAX CtCOIDIO

5391 July 28, 1986APDKll (ATI AHO TIME Or ITAIHC f.T.

As Clairview, P.O. Box 473, Val Caron, Ontario July 23/86 6 ll:15a.mL POM 3AO [x

H5 |f

is•ii!


RESERVATIONS — 400 fOOT SUWACE (MOOT* HE8ERVATWN AROUND ALL LAKES AND MVEM IANO AND OHAVEL W*EKVEO. KAT WSEmCO.

DATE •*Tt•OIK

FILE NO

S. 943188

r This Abstract is a copy of the enfries in the


DEC 2 y 19sbV . /^

Ad~^a-*-LS\^fiffi*^^^^~ffI'StwatfRv^.H'viNa.'WVfiao^-^c^ ' |

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*

•tctirr no.

'

flfl/CQC \JLSinaMinn l ***~"*t H Hi D OD o™** 1 Th* Mining Act S. 94 3207• tCOIDID 1* TH( HAH! Or LICCIICI *0. tlCeiPt HO. (MI (ICOHDIO

EDWARD A. JEROME C. 32301 5391 July 28, 1986• DDIItl (ATI AH* Tint Or ITAIIHt - P.T.

Al5 Clairview, P.O. Box 473, Val Caron, Ontario July 23/86 @ l:10p.m. POM 3AO x

* c

li li• S

ernes u*i OMLV *ECO!DCD •*'-* liet

DATE • ATI *O*K

OKSCVIPTION Of CLAIM


RESERVATIONS — CO fOOT tUMFACt MIOHTB RESERVATION ABOUND AU LAKES AND RIVERS •AND AND (MAVEL MEMftVCD. PEAT RESERVED


FILE NO.

S. 943188

[nis Abstract is a copy of the entries m theRecord Book and is not to oe considered BC assurance ol the validity ol the claim.

^OEC 2 9/&5JP

7^ U ININfif W*We.S MiNtNG'R-jCCRDER , :

SUDBURY MINING DIVISION ^ . , i r-.., j

'

RfCCIPT (0.

r

MOIV8O)

447697 i \j l Norihefn DGnwlopmoflt , CUUMNQ. onuno me* ! Th* Mining Act S. 94 3208

REGINALD J. CHARRONiODICII

^Pbz Drive, Hanmer, Ontario

m 9

Sil tt w

li to

li

orrtct ut* ONLY

0*TI •O*K

L1CINCI "0. IICIIH *0.

:. 29749 5391

POM 1YO

• ATIItCOIDO

tALA*C( ""CilPIIOM Of CLAIM

•ATI IICOKIt

July 28, 1986•ATI Ant Tine Of ITAKIIIC ' f.T.

July 23/86 8 8:00a.m.|x

SCADDING TWP. {G. 3056)

RESERVATIONS — 400 FOOT SURFACE WOHTS RESERVATK9N AROUND AU. LAKES AND RTVEHS SAND AND GRAVEL RESERVED. KAT RESERVEO.

FILE NO.

S. 9432

MI;? rtusiraci is a copy or inc entries m me Record Book and is not to be considered is assurance of the validity of the claim.

8EC 2 y l&tfJ)y /T^J^X

^^J^t\^X-ZX-^^C^

REcqwrtNQ MINING R5CORDHR SUDBURY MINING DIVISION ^'!

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--

08Mam 1 0.

K

1

J

3

447698 001100 ,.'ne* ! Th* Winino Act ' |

REGINALD J. CHARRON iACBRttl

^^z Drive, Hanmer, Ontario

t!s?5"• S

KE*

l!

erncc use ONLY

DATE

'

• ATI •OK K

-

S.943'3o9^^rLICCMCI MO. llCttM BO. DAT! (ICOIDEB . ,- 1 . --. ,.

:. 29749 5391 July 28, 1986 "''•ATI AMB TIBC Or STAND* . . . *.f.

POM 1YO July 23/86 @ 9t35a.m.jx

DATI RECORDED

lAlANCE ""AIPJIO* Or CiAIB- . ;


~ *ANO AND ONAVEL IKSEHVED. PEAT PIEI

^^^^^^THIS Abstract is a copy of the entries in the Record Book and is not to he considered as

IAHOUM)AU.UKESANOmBCk - i EDVEO.

F ILE NO

S. 943208


utu 2 y tomj^f^^a^^^

53BNINOnecoRDU.... . ••VIIMQ oproRDER

SUUlWRY'MrHlNG DIVISION ' J

.

;'V4t

: "-v^'

- --:,^|.~ .'•"" : ^

v: Mi

'.- . ".4"

RECEIPT BO.

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F

-^ifcISIS'•#^.IKS

M^:'{.•'..''.--"

MOIVS01

A K ~7 C O Q - lYr'J Northern Development " IOMMMO. ***MOOy oS* arx3Mines 1 Th. Mining Act 1 S. 943210

REGINALD J. CHARRON :. 29749tBOIKt

^^ez Drive, Hanmer, Ontario POM 1YO

ernci uit ONLY motet* M""e* B""'"

i!i!ttli

DATE

^

Dirt•omc

tICIiri HO. ftATI KCOHK

5391 Julv 28* 1 986•ATI Ad* Tint Of ITAIIII* f. T.

July 23/86 6 ll:15a.m.|xon or CLAIM :


RESERVATIONS — 400 FOOT SURFACE MMTB RESERVATION AKXMO ALL LAKES AND NVtMS. ! •AND AND OMVEL MSERVEO. PEAT fCKMVEO.

1


FUND.

Fnls AhstracTis a copy of the entries in the Record Book and is not to be considered passurance of the validity of the claim.

/^'^^

lASnoeaj MINING RECORD???; dltiJUUKT MKJIH'j DIVISION ' j

-

Oft•cciirT no.

MO (VHA


Appendix II

Location of Diamond Drill Holes

SKETCH SHOWING LOCATION OF RATHBUN LAKE PROSPECTRelative to

ORECO MINES i E NERGY CORP. - WANAPITEI CLAIM GROUP

Scale 1:50 000

RATHBUN LAKE PROSPECT Cu, Ni, Pt, Au

46 0 45'N

Seagull I sland ft

ly ORECO MINES S ENERGY CORP. WANAPITEI CLAIM GROUP -l

j^l\ SCADDING TOWNSHIP .^-'

x

x.\\

X x.1'^x

x

^*f''

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s- '^ '

t******

•w

tasel'nei

i*x

xx\\\\ ai, iiii

i ^

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a—— -1 i

1 1rit/ —————

From Figure 7, Meyer, W., Dec. 28, 1984for Arthurian Resources Limited -Report on an Exploration Program for Gold on the Company'sScadding Township Property, Sudbury Mining Division, Ontario Assessment Files, Ministry of Northern Development S MinesSudbury.

1 /'S 9 4 3 1 9 7 .jsy

. (Formerly S 648522) V

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———————— i ———————— ——— ..

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ORECO MINES S ENERGY CORP.Scadding Township


LOCATION OF DIAMOND DRILL HOLES Claim S 943197

Scale 1 :2400

41I1BNE9365 63.5143 SCADDING 900

m

on 9 7- g-c- 1f?

THIS SUBMITTAL CONSISTED OF VARIOUS REPORTS, SOME OF WHICH HAVE BEEN CULLED FROM THIS FILE. THE CULLED MATERIAL HAD BEEN PREVIOUSLY SUBMITTED UNDER THE FOLLOWING RECORD SERIES (THE DXUMENTS CAN BE VIEWED IN THESE SERIES):

See

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oreco mines s energy corp. - ontario · 2017. 1. 17. · arthurian resources limited held the...

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