| Locality type: | Mine Zone |
| Classification |
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| Species: | Millerite |
| Formula: | NiS |
| Confirmation |
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| Validity: | Believed Valid |
| Data |
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| Mineral Data: | Click here to view Millerite data |
| Locality Data: | Click here to view Amy Lake zone, Capreol Township, Greater Sudbury, Ontario, Canada |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 1286436 |
| Long-form Identifier: | 1:3:1286436:8 |
| GUID (UUID V4): | f57cbbe8-7603-47e7-85bf-eb2efbaa8b5f |
| Nearest other occurrences of Millerite |
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| 1.7km (1.0 miles) | ⓘCapre Lake Mine, Capreol Township, Greater Sudbury, Ontario, Canada |
| 4.3km (2.7 miles) | ⓘBlue Lake Victor Mine, Sudbury area, McKim Township, Greater Sudbury, Ontario, Canada |
| 5.2km (3.2 miles) | ⓘVictor Deep Mine, Maclennan Township, Greater Sudbury, Ontario, Canada |
| 5.3km (3.3 miles) | ⓘMaclennan Mine, Maclennan Township, Greater Sudbury, Ontario, Canada |
| 5.3km (3.3 miles) | ⓘNickel Rim Mine, Maclennan Township, Greater Sudbury, Ontario, Canada |
| 7.2km (4.5 miles) | ⓘWhistle Mine, Norman Township, Greater Sudbury, Ontario, Canada |
| 7.5km (4.7 miles) | ⓘNorman Property, Norman Township, Greater Sudbury, Ontario, Canada |
| 15.3km (9.5 miles) | ⓘDolmac Mine, Rathbun Township, Greater Sudbury, Ontario, Canada |
| 15.7km (9.8 miles) | ⓘBroken Hammer Deposit, Wisner Township, Greater Sudbury, Ontario, Canada |
| 16.2km (10.1 miles) | ⓘGarson Mine, Garson Township, Greater Sudbury, Ontario, Canada |
| References |
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Péntek, A., Molnár, F., Tuba, G., Watkinson, D. H., & Jones, P. C. (2013). The significance of partial melting processes in hydrothermal low sulfide Cu-Ni-PGE mineralization within the footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108(1), 59-78. |
| Reference Search (possible matching items) |
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 | Tuba, Györgyi, Molnár, Ferenc, Ames, Doreen E., Péntek, Attila, Watkinson, David H., Jones, Peter C. (2014) Multi-stage hydrothermal processes involved in “low-sulfide” Cu(–Ni)–PGE mineralization in the footwall of the Sudbury Igneous Complex (Canada): Amy Lake PGE zone, East Range. Mineralium Deposita, 49 (1) 7-47 doi:10.1007/s00126-013-0468-1 | Journal (article/letter/editorial) | | mineralization in the footwall of the Sudbury Igneous Complex (Canada): Amy Lake PGE zone, East Range Györgyi Tuba...Springer-Verlag Berlin Heidelberg 2013 Abstract The Amy Lake PGE zone is a “low-sulfide-type” Cu-(Ni-)PGE mineralization...footwall of the 1.85 Ga Sudbury Igneous Complex occurring in a 100m-wide Sudbury Breccia belt that coincides...coincides with an impactrelated major fracture zone (Bay Fault zone). Detailed hydrothermal alteration mapping...multi-source, multi-stage Sudbury-related hydrothermal system. The two major stages of syn-Sudbury hydrothermal activity |  | Péntek, Attila, Molnár, Ferenc, Tuba, Györgyi, Watkinson, David H., Jones, Peter C. (2013) The Significance of Partial Melting Processes in Hydrothermal Low Sulfide Cu-Ni-PGE Mineralization Within the Footwall of the Sudbury Igneous Complex, Ontario, Canada. Economic Geology, 108 (1) 59-78 doi:10.2113/econgeo.108.1.59 | Journal (article/letter/editorial) | | Mineralization Within the Footwall of the Sudbury Igneous Complex, Ontario, Canada ATTILA PÉNTEK,1,† FERENC MOLNÁR...Mining Company Ltd., 129 Fielding Road, Lively, Ontario, Canada P3Y 1L7 2 Geological 3 Department Survey...Carleton University, 1125 Colonel By Drive, Ottawa, Canada K1S 5B6 Abstract We present new results and review...mineralizing processes in the contact aureole of the Sudbury Igneous Complex. At the basal contact of the igneous...sulfides occurred. In the deeper footwall of the Sudbury Igneous Complex, similar footwall granophyres occur |  | Péntek, Attila, Molnár, Ferenc, Watkinson, David H., Jones, Peter C., Mogessie, Aberra (2011) Partial melting and melt segregation in footwall units within the contact aureole of the Sudbury Igneous Complex (North and East Ranges, Sudbury structure), with implications for their relationship to footwall Cu–Ni–PGE mineralization. International Geology Review, 53 (2) 291-325 doi:10.1080/00206810903101313 | Journal (article/letter/editorial) | | contact aureole of the Sudbury Igneous Complex (North and East Ranges, Sudbury structure), with implications...Carleton University, 1125 Colonel By Drive, Ottawa, Canada, K1S 5B6; cInstitute for Earth Sciences, Karl-Franzens...the contact aureole of the Sudbury Igneous Complex (SIC) in the 1.85 Ga Sudbury impact structure. Our results...results, derived from mapping within the North (Windy Lake, Foy, Wisner areas) and East Ranges (Skynner, Frost...Wisner area and up to 9008C in the Frost and Windy Lake areas. Segregations of partial melt into veins and |
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