| Locality type: | Prospect |
| Classification |
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| Species: | Pyrrhotite |
| Formula: | Fe1-xS |
| Confirmation |
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| Validity: | Believed Valid |
| Data |
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| Mineral Data: | Click here to view Pyrrhotite data |
| Locality Data: | Click here to view Franklin prospect, Slate Creek Mining District, Shoshone County, Idaho, USA |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 447072 |
| Long-form Identifier: | 1:3:447072:4 |
| GUID (UUID V4): | 4778d5b5-800e-440a-b2e7-cdf93069045e |
| Nearest other occurrences of Pyrrhotite |
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| 7.4km (4.6 miles) | ⓘCougar group, Black Prince Mining District, Shoshone County, Idaho, USA |
| 7.6km (4.7 miles) | ⓘCougar prospect, Black Prince Mining District, Shoshone County, Idaho, USA |
| 10.4km (6.5 miles) | ⓘCopper Prince Mine, Black Prince Mining District, Shoshone County, Idaho, USA |
| 20.4km (12.7 miles) | ⓘMorning No. 6 adit, Hunter Mining District, Shoshone County, Idaho, USA |
| 21.9km (13.6 miles) | ⓘLucky Friday Mine, Hunter Mining District, Shoshone County, Idaho, USA |
| 23.2km (14.4 miles) | ⓘMorning Mine, Hunter Mining District, Shoshone County, Idaho, USA |
| 23.6km (14.7 miles) | ⓘHelena-Frisco Mine, Lelande Mining District, Shoshone County, Idaho, USA |
| 23.8km (14.8 miles) | ⓘFrisco Mine, Lelande Mining District, Shoshone County, Idaho, USA |
| 24.2km (15.0 miles) | ⓘBlack Bear Fraction Mine, Lelande Mining District, Shoshone County, Idaho, USA |
| 24.2km (15.0 miles) | ⓘConstitution Mine, Pine Creek Mining District, Shoshone County, Idaho, USA |
| References |
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| Reference Search (possible matching items) |
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 | Duuring, Paul, Hassan, Lee, Zelic, Mario, Gessner, Klaus (2016) Geochemical and Spectral Footprint of Metamorphosed and Deformed VMS-style Mineralization in the Quinns District, Yilgarn Craton, Western Australia*. Economic Geology, 111 (6) 1411-1438 doi:10.2113/econgeo.111.6.1411 | Journal (article/letter/editorial) | | Deformed VMS-style Mineralization in the Quinns District, Yilgarn Craton, Western Australia* Paul Duuring...massive sulfide (VMS) occurrences in the Quinns district are hosted predominantly by ca. 2814–2800 Ma banded...geochemistry. Rhyolite exposed throughout the district and intersected by drill holes records distal...the Austin deposit in the western part of the district, abundant talc and anthophyllite with minor cummingtonite...known VMS prospects in the eastern half of the district, the rhyolite grades into a 2 × 1 km zone of schistose |
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