41I10SW2009 2.23781 GARSON 010 2 .2378 l
Petrological Study
on part of the
Sudbury Breccia Belt #2 Claim Group N.T.S.41I/11 SW
For
Wallbridge Mining Company Limited
Patrick Toth, B.Se. June 18, 2002
Table of Contents
Introduction..........................................................................................................................................................!
Location and Access ............................................................................................................................................J
Property History...................................................................................................................................................4
Topography.........................................................................................................................
Regional Geology.................................................................................................................................................^
Property Geology..................................................................................................................................................6
Exploration Surveys .............................................................................................................................................6
Conclusions and Recommendations....................................................................................................................6
Bibliography .........................................................................................................................................................7
Statement of Qualifications .................................................................................................................................8
List of Figures
Figure l: General Location Map Page 2 Figure 2: Property Location Map Page 3
Map Pocket
Geology and Sample Location Map
List of Tables
Table l: Claim Status Page l Table 2: Lithological Units Page 5
List of Appendices
Appendix A: Petrological Results
Appendix B: Assay Results
Introduction
On June 4th and 5 th of 2002, geological traverses were conducted across the Eastern block of the Sudbury Breccia Belt #2 claim group. The purpose was to locate and sample any Sudbury Breccia encountered for petrographic description and to verify the validity of previous mapping. Four rock types; arkose, greywacke, gabbro and false volcanics were encountered. 15 samples were collected for assay and petrological purposes.
Location and Access
The property is located in the northeastern corner of the Town of Sudbury, Ontario and is encompasses part of the Timberwolf Golf and Country Club. The claim block comprises Lot l, Con l, of Garson Township (figures l Si 2). The property can be most easily accessed by traveling east towards Garson along Hwy 86 and turning north onto Donnelly Drive. Follow Donnelly Drive north to O'Neil Drive West and turn left. Travel west for another 2 kilometers and cross over a set of railroad tracks. At this point, a foot trail heads southwest to the power line and the golf course. Walking west along the power line for approximately 100 metres bring one to the eastern claim boundary.
Claim Status
Property Name:Principal Commodity of Interest:Location:Township:Mining District:Province:Date of Acquisition:Renewal Dates:Operators Names:Title Status:
Sudbury Breccia Belt #2 GroupNi, Cu, and PGE'sLot 1J Con lGarsonSudburyOntarioJune22, 1999June 22, 2002Wallbridge Mining CompanyThe claims are wholly owned and are in good standing.
Table l: Claim Status
Claim #1222978
Size (units)7
Recording DateJune 22, 1999
Due DateJune 22, 2002
Figure 1: General Location Map
SRBB#2 CLAIM
Ontario
Figure 2: Property Location Map
LOT1
Lot 12
Con l
1222978
11
Property History
No past prospecting or mining activity has been recorded on the claim.
Topography
The property is generally flat with the exception of a large east-west outcrop ridge located along the northern portions of the claim block. Outcrop exposure consists of several small to medium-sized outcrops and outcrop ridges of low relief. The outcrop areas are largely devoid of overburden and any substantial vegetation. Overburden depth is generally very shallow. The southern portion of the claim block is low and comprises the Timberwolf Golf and Country Club.
Regional Geology
The Sudbury Igneous Complex is interpreted to have originally been a 200km diameter melt crater. The present expression of the now deformed crater is an elliptical form 65km long by 35km wide. It hosts some of the largest nickel-copper-PGE ore bodies found in the world. The geological history of the Complex has blessed it with numerous geologically diverse settings for the emplacement of nickel-copper-PGE deposits.
There are numerous volumes written about the Sudbury Structure and a more complete description of the geology can be found in the OGS Special Volume l, The Geology and Ore Deposits of the Sudbury Structure, 1984, edited by E. G. Pye, A. J. Naldrett and P.E. Giblin.
The 1850 Ma Sudbury Structure is located just northwest of the Grenville Geological Province, at the present boundary of the Superior Geological Province and the Southern Geological Province. The melt rocks associated with the structure consist of several basal units, some of which are critical to the deposition of sulphide ore bodies.
The "Main Mass" rocks consist of norite, quartz gabbro and granophyre while fine- to medium-grained quartz diorite and mafic norite breccias form the "Sublayer" at its base. The sublayer is host to much of the Ni-Cu sulphide ores of the Sudbury Structure which are emplaced in embayments at the contact with the crater walls. Granite breccias occurring at the base of the embayments also host the sulphides. Discrete radial and concentric offset dikes host nickel-copper-PGE deposits in a matrix of quartz diorite and associated breccias.
The impact at Sudbury formed pseudotachylytes (Sudbury Breccia) veins, melt bodies and Footwall Breccias that also contain appreciable economic mineralization. Differentiated sulphides rich in copper and PGE's are often found trapped in brecciated footwall rocks hosting Sudbury Breccia units and related melt bodies.
The basal units are overlain by various heterolithic breccias of the Onaping Formation and fluvial sediments of the Onwatin and Chelmsford Formations.
The Sudbury Structure has been deformed into its present day elliptical shape by northwesterly directed thrusting followed by regional metamorphism during the Leonean Orogeny. The 37Ma Wanapitei Lake Crater east of the Sudbury Structure also deformed the basin to its present shape.
Table 2 provides an overview of the numerous lithological units encountered in the Sudbury Igneous Complex.
Table 2: Table of LithologicalUnits
PHANEROZOICCENOZOIC
QUATERNARYRECENT
Organic deposits (peat bog); floodplain (alluvial) deposits
PLEISTOCENEGlacial deposits, glaciofluvial deposits, glaciolacustrine deposits
UNCONFORMITY
PROTEROZOIC
ARCHEAN
Olivine DiabaseINTRUSIVE CONTACT
Trap DikesINTRUSIVE CONTACT
Sudbury Igneous ComplexSublayerINTRUSIVE CONTACT Main Mass Gabbro
Whitewater GroupChelmsford Formation Onwatin Formation Onaping Formation
Black Member Grey Member Basal Member
Sudbury Breccia Footwall Breccia Shock Metamorphism
SUDBURYEVENT Nipissing Intrusive Rocks
INTRUSIVE CONTACT Creighton and Murray Granites
INTRUSIVE CONTACT Huronian Supergroup
Copper Cliff Formation UNCONFORMITY
DiabaseINTRUSIVE CONTACT
Mafic Plutonic Rocks and Anorthosite Intrusive; Contact Migmatite and Felsic Plutonic Rocks
INTRUSIVE (fe METAMORPHIC CONTACTMetavolcanic and Metasedimentary Rocks; Granodioritic-Quartzdioritic Gneisses and Associated Mafic Rocks
Property Geology
The Sudbury Breccia Belt #2 Property parallels the Sudbury Igneous Complex (SIC) over a strike length of 400m and is situated approximately 2.5km south of the SIC contact. The property overlays the South Range footwall rocks of the SIC. These are represented by the felsic meta-volcanics of the Copper Cliff Formation ^2460 Ma.). This formation is a member of the Huronian Supergroup (2100 to 2500 Ma.) and of the Elliot Lake Group respectively.
The property for the most part, is underlain by feldspathic wackes, quartz arenites and mafic flows of the Stobie Formation. Minor outcroppings of felsic tuffs of the Copper Cliff Formation can be observed in the middle of the claim block. Sudbury Breccia is also present in large quantities and can be most readily observed cutting the metasedimentary units. Metamorphism in the area ranges from lower-greenschist to amphibolite facies.
The metasediments weather brown weathered surface and a dark-gray in fresh surface. Grain size varies from fine to medium. Local cross bedding and grading are present as are minor polymictic and oligomictic pebble conglomerate beds. The metasediments have a granoblastic texture and contain porphyroblasts of hornblende, garnet and staurolite. Gabbro intrudes the metasedimentary and felsic volcanic rocks. The gabbro is generally dark green, medium to coarse-grained and is comprised of euhedral to subhedral amphiboles in a granoblastic matrix of feldspar, quartz and amphibole, chlorite and epidote. Hornblende occurs as radiating porphyroblasts and subhedral poikiloblasts. Trace amounts of pyrite and pyrrhotite are present.
Exploration Surveys
On June 4th and 5th , the eastern block of the Sudbury Breccia Belt #2 claim group was traversed and sampled. The work consisted of observing the outcrops traversed and taking grab samples of any Sudbury Breccia encountered for petrological and assay analysis.
Fifteen samples for petrological and assay purposes were taken at various outcrops on the claim block (map pocket). Samples PT-02-006 and 007 were described as narrow bands of Sudbury Breccia cutting greywacke. Sample PT-02-008 was described as a strongly foliated Sudbury Breccia in a well-bedded greywacke. PT-02- 009 was described as medium to coarse-grained, gabbro with radiating hornblende crystals. Sample PT-02-010 and 011 were described as strongly foliated Sudbury Breccias in greywacke. Sample PT-02-012 was described as a fine-grained, greywacke or quartz arenite. Sample PT-02-013 was described as a possible Sudbury Breccia in greywacke. Sample PT-02-014 was described as a medium-grained gabbro/amphibolite. Sample PT-02-015 was described as Sudbury Breccia in greywacke. Sample PT-02-016 was described as a medium to coarse- grained gabbro/amphibolite. Sample PT-02-017 was described as fine to medium-grained gabbro/amphibolite with possible Sudbury Breccia. Sample PT-02-018 was described as a strongly foliated, fine-grained gabbro. Sample PT-02-019 was described as a foliated and schistose greywacke with possible Sudbury Breccia. Sample PT-02-020 was described as a fine to medium-grained gabbro. The samples were cut, examined and areas to be thin sectioned were selected with the remaining portions being sent for assay. A detailed description of the petrographic work and the assay results can be found in Appendices A and B respectively.
Conclusions and Recommendations
Of the fifteen samples taken; 7 were Sudbury Breccia, 7 were gabbro/amphibolite and l was an arkosic metasediment. No significant assay values were returned. The Sudbury Breccias upon microscopic examination were found to be relatively "warm" in nature with textures ranging from fine-grained porphyritic to recrystallized. Given the large quantity of Sudbury Breccia on the property in conjunction with its close proximity to the known limit of the Sudbury Breccia Belt and several producing and past producing mines, a Total Field Magnetic survey might be warranted.
Bibliography
Card, K. D., Gupta V. K., McGrath, P. H., and Grant, F. S. 1984: The Sudbury Structure: it's regionalgeological and geophysical setting. In: The Geology and Ore Deposits of the Sudbury Structure. Ontario Geological Survey special volume l.
Dressler, B.O., Gupta, V.K. and Muir, T.L. 1991: The Sudbury Structure; in Geology of Ontario, Ontario Geological Survey, Special Volume 4, Part l, pp. 593-625.
Dressler, B.O. 1984: Chapter 4, General Geology of the Sudbury Area; in The Geology and Ore Deposits of the Sudbury Structure, Ontario Geological, Special Volume l, pp.57-82.
Innes, D.G. 1978: McKim Township, District of Sudbury; Ontario Geological Survey Prelim. Map P. 1978, Geol. Sen, scale 1:15840 or l inch to '/4 mile. Geology 1975, 1976.
John, G.W. 1996: Precambrian geology of Garson and Blezard townships; Ontario Geological Survey, Open File Report 5950, 47p.
Statement of Qualifications
I Patrick E. Toth, of the City of Toronto, in the Province of Ontario, Canada, do hereby certify that:
1. I am an exploration geologist residing at 42 Nursewood Road, Toronto, Ontario, M4E 3R8
2. I hold a B.Se., Geological Sciences degree conferred by Brock University of St. Catharines, Ontario in 1995.
3. I have practiced as an exploration geologist since 1995.
4. I am a member of the Geological Association of Canada, Canadian Prospectors and Developers Association of Canada, and The Canadian Institute of Mining and Metallurgy and Petroleum.
5. This report is based on personal examination and the implementation of work on the property on the dates of June 4th and 5th, 2002 on behalf on Wallbridge Mining Company.
6. I have no direct interest in the properties or securities of Wallbridge Mining Company.
Dated at Sudbury, Ontario,
this 18th Day of June, 2002 Patrick E. Toth, B.Sc.
Appendix A
Petrographic Descriptions
Sample # PT-02-006 Thin Section # W-02-0180
Hand Specimen Description: Narrow band of warm Sudbury Breccia cutting greywacke. Local gabbro raftswithin the greywacke.
Thin Section Description: Sudbury Breccia with abundant plagioclase spicules. Matrix is of intermediatecomposition with gabbroic/dioritic and sedimentary fragments and a fine grained, porphyritic texture.
Sample # PT-02-007 Thin Section # W-02-0181
Hand Specimen Description: Narrow band of warm Sudbury Breccia cutting greywacke. Local gabbro raftswithin the greywacke.
Thin Section Description: Sudbury Breccia with lineated plagioclase crystals. Matrix is of intermediatecomposition with sedimentary fragments and a fine-grained, porphyritic texture.
Sample # PT-02-008 Thin Section* W-02-0182
Hand Specimen Description: A strongly foliated Sudbury Breccia in a well bedded greywacke.
Thin Section Description: A strongly foliated Sudbury Breccia. Matrix is of intermediate compositionwith sedimentary fragments and a recrystallized texture.
Sample # PT-02-009 Thin Section # W-02-0183
Hand Specimen Description: A medium to coarse-grained gabbro with radiating hornblende crystals.
Thin Section Description: Coarse-grained, quartz-amphibolite. Quartz and feldspars crystals are in a fine grained mosaic with relict, sub-ophitic texture.
Sample # PT-02-010 Thin Section # W-02-0184
Hand Specimen Description: A strongly foliated Sudbury Breccia in a greywacke raft within gabbro.
Thin Section Description: A strongly foliated Sudbury Breccia. Matrix is of intermediate compositionwith sedimentary fragments and a fine-grained, porphyritic to recrystallized texture.
Sample # PT-02-011 Thin Section # W-02-0185
Hand Specimen Description: A strongly foliated Sudbury Breccia in a greywacke raft within gabbro.
Thin Section Description: A moderately lineated Sudbury Breccia. Matrix is of intermediate compositionwith sedimentary and gabbroic fragments and a fine-grained, porphyritic to recrystallized texture.
Sample # PT-02-012 Thin Section # W-02-0186
Hand Specimen Description: A fine-grained greywacke or quartz-arenite.
Thin Section Description: Fine-grained, biotite-quartz amphibolite.
Sample # PT-02-013 Thin Section # W-02-0187
Hand Specimen Description: Possible Sudbury Breccia in greywacke.
Thin Section Description: Fine to medium-grained, arkosic metasediment.
Sample # PT-02-014 Thin Section # W-02-0188
Hand Specimen Description: Medium-grained gabbro/amphibolite in contact with greywacke containingminor amounts of Sudbury Breccia.
Thin Section Description: Hornfelzed, oxide-rich, biotite-amphibolite.
Sample # PT-02-015 Thin Section # W-02-0189
Hand Specimen Description: Sudbury Breccia in greywacke.
Thin Section Description: Sudbury Breccia with a matrix of intermediate composition, sedimentaryfragments and a fine-grained, porphyritic texture.
Sample # PT-02-016 Thin Section # W-02-0190
Hand Specimen Description: A medium-grained, gabbro/amphibolite.
Thin Section Description: A weakly sheared, coarse-grained, quartz-hornblendite.
Sample # PT-02-017 Thin Section # W-02-0191
Hand Specimen Description: A fine to medium-grained gabbro with possible Sudbury Breccia.
Thin Section Description: A biotite-quartz-amphibolite with porphyritic hornblende crystals.
Sample # PT-02-018 Thin Section # W-02-0192
Hand Specimen Description: A strongly foliated, fine-grained gabbro with possible Sudbury Breccia.
Thin Section Description: Sudbury Breccia. Matrix is of intermediate composition with sedimentary andgabbroic fragments and a recrystallized texture in contact with a recrystallized, sub-ophitic quartz-amphibolite.
Sample # PT-02-019 Thin Section # W-02-0193
Hand Specimen Description: A foliated, schistose greywacke with possible Sudbury Breccia.
Thin Section Description: A recrystallized, medium-grained, biotite-amphibolite.
Sample # PT-02-020 Thin Section # W-02-0194
Hand Specimen Description: A fine to medium-grained gabbro.
Thin Section Description: A fine to medium-grained, recrystallized amphibolite-rich biotite-amphibolite.
Appendix B
Assay Results
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Work Order: 068244 Date: 19/06/02 PRELIMINARY Page l of 3
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Element. Method. Det.Lim. Units.
W ALI 601 WAL1602 WALI603 WAL1604 WAL1605
W ALI 606 W ALI 607 WAL1608 WAL1609 WAL1610
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ONTMUO MINISTRY OF NORTHERN DEVELOPMENT AND MINES
Transaction No: W0270.01055
Recording Date: 2002-JUN-20
Approval Date: 2002-SEP-19
Work Report Summary
Status: APPROVED
Work Done from : 2002-MAY-15
to: 2002-JUN-19
Client(s):
392385
Survey Type(s):
WALLBRIDGE MINING COMPANY LIMITED
ASSAY MICRO
Work Report Details:
Perform Claim* Perform Approve
S 1222978 S3,530 S3.530 53,530 S3,530
Applied Approve
SO
Assign ReserveApprove Reserve Approve Due Date
O SO SO 2003-JUN-22
S3, 530 S3.530 S3.530 S3.530 SO SO SO SO
External Credits:
Reserve:
SO
SO Reserve of Work Report#: W0270.01055
SO Total Remaining
Status of claim is based on information currently on record.
41I10SW2009 2.23781 GARSON 900
2002-Sep-19 16:12 Armstrongjd Page 1 of 1
Ministry ofNorthern Developmentand Mines
Date:2002-SEP-19
Ministers du Developpement du Nord et des Mines Ontario
GEOSCIENCE ASSESSMENT OFFICE 933 RAMSEY LAKE ROAD, 6th FLOOR SUDBURY, ONTARIO P3E 6B5
WALLBRIDGE MINING COMPANY LIMITED 129 FIELDING ROAD LIVELY, ONTARIO P3Y 1L7 CANADA
Tel: (888) 415-9845 Fax:(877)670-1555
Dear Sir or Madam
Submission Number: 2.23781 Transaction Number(s): W0270.01055
Subject: Approval of Assessment Work
We have approved your Assessment Work Submission with the above noted Transaction Number(s). The attached Work Report Summary indicates the results of the approval.
At the discretion of the Ministry, the assessment work performed on the mining lands noted in this work report may be subject to inspection and/or investigation at any time.
If you have any question regarding this correspondence, please contact LUCILLE JEROME by email at [email protected] or by phone at (705) 670-5858.
Yours Sincerely,
Ron Gashinski
Senior Manager, Mining Lands Section
Gc: Resident Geologist
Mark Hall (Agent)
Assessment File Library
Wallbridge Mining Company Limited (Claim Holder)
Wallbridge Mining Company Limited (Assessment Office)
Visit our website at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:17541
MINING LAND TENURE
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ADMINISTRATIVE DISTRICTS ; DIVISIONSMining Division Sudbury
Land Titles'Reglstry Division SUDBURY
Ministry of Natural Resources Ditlrict SUDBURY
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