| Locality type: | Mine |
| Classification |
|---|
|
| Species: | Acanthite |
| Formula: | Ag2S |
| Confirmation |
|---|
|
| Validity: | Believed Valid |
| Data |
|---|
|
| Mineral Data: | Click here to view Acanthite data |
| Locality Data: | Click here to view Silver King Mine 1 (Silver King), Drake, Drake Co., New South Wales, Australia |
| Data Identifiers |
|---|
|
| Mindat Occurrence Record ID: | 229966 |
| Long-form Identifier: | 1:3:229966:2 |
| GUID (UUID V4): | 67660b11-d03a-405b-8f8b-046a2c3fab05 |
| Nearest other occurrences of Acanthite |
|---|
|
|
| 0.8km (0.5 miles) | ⓘLady Hampden Pit (Lady Hampden Mine), Drake, Drake Co., New South Wales, Australia |
| 1.4km (0.9 miles) | ⓘDrake, Drake Co., New South Wales, Australia |
| 13.4km (8.3 miles) | ⓘGolden Crown reef 2, Drake district, Buller Co., New South Wales, Australia |
| 13.6km (8.4 miles) | ⓘAddisons Mine (Addisons reef), Drake district, Buller Co., New South Wales, Australia |
| 14.0km (8.7 miles) | ⓘGolden Age Mine (Silver Age mine; Mariners; No 1 Golden Age south), Drake district, Buller Co., New South Wales, Australia |
| 32.5km (20.2 miles) | ⓘWatt & Co prospect, Wilsons Downfall, Buller Co., New South Wales, Australia |
| 94.2km (58.5 miles) | ⓘWebbs Silver Mine (Webbs Mine; Collisons silver Mine; Bates copper lode; The Little Plant; White Rock silver Mine), Emmaville, Gough Co., New South Wales, Australia |
| References |
|---|
|
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) |
|---|
 | 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 |
|
