| Locality type: | Mine |
| Classification |
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| Species: | Polybasite |
| Formula: | [Ag6Sb2S7][Ag9CuS4] |
| Confirmation |
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| Validity: | Believed Valid |
| Data |
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| Mineral Data: | Click here to view Polybasite data |
| Locality Data: | Click here to view Silver King Mine 1 (Silver King), Drake, Drake Co., New South Wales, Australia |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 893931 |
| Long-form Identifier: | 1:3:893931:9 |
| GUID (UUID V4): | 14c404bc-3430-4666-b4a3-4c630dab4cb2 |
| Nearest other occurrences of Polybasite |
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| 0.8km (0.5 miles) | ⓘLady Hampden Pit (Lady Hampden Mine), Drake, Drake Co., New South Wales, Australia |
| 1.3km (0.8 miles) | ⓘStrauss Deposit, Drake, Drake Co., New South Wales, Australia |
| 4.0km (2.5 miles) | ⓘMascotte Mine (Mascotte reef), Drake, Drake Co., New South Wales, Australia |
| 5.1km (3.2 miles) | ⓘBorder Chief Mine, Drake district, Buller Co., New South Wales, Australia |
| 13.4km (8.3 miles) | ⓘGolden Crown reef 2, Drake district, Buller Co., New South Wales, Australia |
| 22.7km (14.1 miles) | ⓘAnnie reef (Annie Mine; Isobel Mine; Vickerys reef; Claverie & Nelmes Mine), Tenterfield district, Buller Co., New South Wales, Australia |
| 80.0km (49.7 miles) | ⓘSilver lode (Corbetts prospect), Silent Grove, Clive Co., New South Wales, Australia |
| References |
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Henley, H. F., Brown, R. E., Brownlow, J. W., Barnes, R. G., Stroud, W. J. (2001) Grafton-Maclean Metallogenic Map (SH/56-6, SH/56-7) Metallogenic Study and Mineral Deposit Data Sheets. Geological Survey of New South Wales |
| Reference Search (possible matching items) |
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 | Lynch, J.V.G, Longstaffe, F.J, Nesbitt, B.E (1990) Stable isotopic and fluid inclusion indications of large-scale hydrothermal paleoflow, boiling, and fluid mixing in the Keno Hill Ag-Pb-Zn district, Yukon Territory, Canada. Geochimica et Cosmochimica Acta, 54 (4) 1045-1059 doi:10.1016/0016-7037(90)90438-q | Journal (article/letter/editorial) | | quartz in the orebodies demonstrate an evolving HzO-CO?-NaCl-CH4 system. Loss of COz and CHG during water...lower homogenization temperatures. Quartz from silver-rich veins has been shifted to higher 6180 values...values, by up to 4%0 relative to adjacent silver-poor veins, the result of a minimum 10-25s adiabatic boiling...Kcno Hill vein system which encompass separation of CO-. and c‘HJ from water, during vaporization and cooling...paper. we investigate the effects that boiling ofH@-CO-NaCl i CH4 mineralizing fluids had on the oxygen |
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