Classification |
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Species: | Pyrrhotite |
Formula: | Fe1-xS |
Confirmation |
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Validity: | Confirmed |
Confirmation Methods: | Visually Identified |
Data |
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Mineral Data: | Click here to view Pyrrhotite data |
Locality Data: | Click here to view Vein 113, Nipissing 404, Coleman Township, Cobalt area, Cobalt-Gowganda region, Timiskaming District, Ontario, Canada |
Data Identifiers |
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Mindat Occurrence Record ID: | 1016058 |
Long-form Identifier: | 1:3:1016058:7 |
GUID (UUID V4): | 29f5dcad-1506-4a85-91e6-ff48a83a9f8d |
Nearest other occurrences of Pyrrhotite |
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0.5km (0.3 miles) | ⓘColeman Road roadcut, Coleman Township, Cobalt area, Cobalt-Gowganda region, Timiskaming District, Ontario, Canada |
1.3km (0.8 miles) | ⓘLa Rose Mine, Coleman Township, Cobalt area, Cobalt-Gowganda region, Timiskaming District, Ontario, Canada |
1.6km (1.0 miles) | ⓘO'Brien Mine, Coleman Township, Cobalt area, Cobalt-Gowganda region, Timiskaming District, Ontario, Canada |
1.8km (1.1 miles) | ⓘColonial Mine, Coleman Township, Cobalt area, Cobalt-Gowganda region, Timiskaming District, Ontario, Canada |
1.9km (1.2 miles) | ⓘSilverfields mine (Alexandra mine), Coleman Township, Cobalt area, Cobalt-Gowganda region, Timiskaming District, Ontario, Canada |
1.9km (1.2 miles) | ⓘJuno Mine, Coleman Township, Cobalt area, Cobalt-Gowganda region, Timiskaming District, Ontario, Canada |
1.9km (1.2 miles) | ⓘPenn-Canadian Mine (Cobalt Central; Bailey ; Glen Lake ; Big Pete), Coleman Township, Cobalt area, Cobalt-Gowganda region, Timiskaming District, Ontario, Canada |
2.1km (1.3 miles) | ⓘArgentite mine, Coleman Township, Cobalt area, Cobalt-Gowganda region, Timiskaming District, Ontario, Canada |
2.2km (1.3 miles) | ⓘSilver Cliff Mine, Coleman Township, Cobalt area, Cobalt-Gowganda region, Timiskaming District, Ontario, Canada |
2.2km (1.4 miles) | ⓘWaldman Mine, Gillies Limit, Cobalt area, Cobalt-Gowganda region, Timiskaming District, Ontario, Canada |
References |
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Reference Search (possible matching items) |
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| | Report (issue) | MOLYBDENUM DEPOSITS OF CANADA F. M. Vokes $4.50 1963 MOLYBDENUM DEPOSITS OF CANADA 2,500-1962-1992 56160-5-1...Molybdenite Corporation of Canada, Limited (June 1958). GEOLOGICAL SURVEY OF CANADA ECONOMIC GEOLOGY REPORT...MOLYBDENUM DEPOSITS OF CANADA By F. M. Vokes DEPARTMENT OF MINES AND TECHNICAL SURVEYS CANADA ROGER DUHAMEL...most of the important molybdenum-bearing areas in Canada. Because of the growing interest in molybdenum...J. M. HARRISON, Director, Geological Survey of Canada. OTTAWA, January 5, 1960. v CONTENTS CHAPTER | | | Book | Geology, Lakehead University Thunder Bay, Ontario, P7B 5El, Canada M. BRIAN BA YLY, Professor Department...Spivak at Lakehead v University, Thunder Bay, Ontario. Costs involved by the editors were defrayed by...Natural Sciences and Engineering Research Council of Canada to Graham Borradaile. Beside the people involved... Box 5342, Dunedin, New Zealand BOND, W. D. Ontario Geological Survey, Ministry of Natural Resources...Resources, 77 Grenville Street, Toronto, Ontario M5S IB3, Canada BORRADAILE, GRAHAM JOHN Department of Geology | | Arehart, Greg B., Eldridge, C.Stewart, Chryssoulis, Stephen L., Kesler, Stephen E. (1993) Ion microprobe determination of sulfur isotope variations in iron sulfides from the Post/ Betze sediment-hosted disseminated gold deposit, Nevada, USA. Geochimica et Cosmochimica Acta, 57 (7) 1505-1519 doi:10.1016/0016-7037(93)90010-t | Journal (article/letter/editorial) | MineralogySection, SurfaceScience Western, London, Ontario,Canada N6A 5B8 (Received May 29, 1991; accepted in...*-11? jasphin I -me vein reallorp barite msv I .-(I-* massive vein -113. I stibnite calcite...realgar-calcite vein (white = calcite; light grey = realgar) cutting arsenian pyrite-bearing ore. Vein is s~gni~eant~y...Replafim? PO Re&cin~ -p C-ttinn Lstest vein Croscuttin~ latest vein Replacing po Cube I. p&e px cube Cube...pyrite Vein margin me + preore py Vein margIn mc + preore py Vein me 90 pm from vein wall Vein me 140 | | | Report (volume) | RESOURCES OF THE TRACY ARM-FORDS TERROR WILDERNESS STUDY AREA AND VICINITY, ALASKA FRONTISPIECE.-Oblique aerial...Resources of the Tracy Arm-Fords Terror Wilderness Study Area and Vicinity, Alaska By A. B. C. D. E. F. U...Geology of the Tracy Arm-Fords Terror wilderness study area and vicinity, Alaska Interpretation of the aeromagnetic...Geochemistry of the Tracy Arm-Fords Terror wilderness study area an~ vicinity, Alaska Mineral deposits and occurrences...occurrences in the Tracy Arm-Fords Terror wilderness study area and vicinity, Alaska Evaluation of mineral resources | | | Book (edition) | continued to be won as a by-product. From a restricted area of the field, zinc ore has also been mined. The...Pendleian stage of the Carboniferous system in an area of abc)ut 1700 km 2 ; the incidence of orebodies...Other publications of the Survey dealing with this district and ad_joinin_g districts BOOKS Memoirs Geology...and country around Bellingharr1 the Cross Fell area country around Brough-under-Stainmore country between...details Introductory note 104 Area 1 The Escarpment 104 118 Chapter Area 2 Subarea Subarea 151 Chapter | | | Book | Textures – Channelway Recognition General Approach Vein Styles Breccia Styles Other Styles Miarolitic Igneous...Sulphide-Pyrrhotite Topaz Albite, Chlorite (Granite) 45 45 Structural Style Vein Pipe Stockwork-Vein Miarolitic...Breccia-Vein Fault Breccia-Vein Vein Intrusive Breccia Stockwork Breccia Intrusive Breccia Vein Pervasive-Vein-Breccia...Pervasive-Vein-Breccia Vein (Ductile Style) Layer Controlled, Vein Vein Vein Vein Breccia Layer Controlled...Controlled, Vein Fault Breccia-Vein Background, Selective Semi-Pervasive 4 Alteration minerals – Some General | | | Report (volume) | Bedded Ores in England and Wales. Redesdale and district Yorkshire ... Derby-Notts Warwickshire Staffordshire...the CAder Idris region teferred to ilhe pisolitic ironstone of the Llyn-.A.ran district (2½ miles S. by...length, and a large quantity of dis8emina.ted pyrrhotite (magnetic pyrites, Fe6 S 7 ). 'l.'his mineral...Penmorfa Fault, an overthrust that cros~s the district in a direction ranging N. 500 W. from Portmadoc...lenticular masses of pisolitic iron~ore of that district. They occur in assooiation with graptolitic shales |
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