| Deposit ID | 10085924 |
|---|---|
| MRDS ID | W701786 |
| Record type | Site |
| Current site name | Ol'Khovo |
| Geographic coordinates: | 92.00005, 53.99774 (WGS84) |
|---|
Political divisions (FIPS codes)
Russia(country)
Europe(continent)
Land(continent)
| Country |
|---|
| Russia |
| Commodity | Importance |
|---|---|
| Gold | Primary |
| Copper | Secondary |
| Cobalt Critical | Tertiary |
| Bismuth Critical | Tertiary |
| Tellurium Critical | Tertiary |
| Selenium | Tertiary |
| Materials | Type of material |
|---|---|
| Bornite | Ore |
| Chalcocite | Ore |
| Chalcopyrite | Ore |
| Galena | Ore |
| Gold | Ore |
| Hessite | Ore |
| Krennerite | Ore |
| Magnetite | Ore |
| Marcasite | Ore |
| Pyrite | Ore |
| Pyrrhotite | Ore |
| Sphalerite | Ore |
| Tetradymite | Ore |
| Calcite | Gangue |
| Chlorite | Gangue |
| Dolomite | Gangue |
| Quartz | Gangue |
| Sericite | Gangue |
| Serpentine | Gangue |
| Siderite | Gangue |
| Host or associated | Host |
|---|---|
| Rock type | Plutonic Rock > Granitoid > Granite |
| Rock unit name | Ol'Khovo Complex;Chibizhek Group;Osinovo Group |
| Rock description | Ol'Khovo Complex;Chibizhek Group;Osinovo Group |
| (1) | 92.00005, 53.99774 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | In Area Where The Geological Structures Of The East Sayan Anticlinorium Join With The Minusinsk Syneclise |
| Type of structure | Local |
| Structure description | See Comments |
| Development status | Producer |
|---|---|
| Commodity type | Metallic |
| Significant | No |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | W701786 |
SMIRNOV, V.I., ED., 1977, ORE DEPOSITS OF THE USSR (VOLUME III, PAGE 52-55): LONDON, PITMAN PUBLISHING
| Subject category | Comment text |
|---|---|
| Deposit | SHAPE OF ORE BODIES IS VARIED. IN THE CARBONATE ROCKS, SULPHIDE ORE BODIES IN THE FORM OF LENSES, PIPES, AND SHOOT-LIKE SEGREGATIONS, COMPLICATED BY APOPHYSES, ARE DISTRIBUTED DIRECTLY IN THE NORTHWESTERLY-STRIKING FAULT ZONES OR AT THE JUNCTION OR INTERSECTION OF THESE ZONES WITH FAULTS OF OTHER DIRECTIONS. IN THE HORNFELSES, HORNFELSED ROCKS, AND GRANITES, THE MINERALIZATION CONSISTS OF QUARTZOSE AND QUARTZ-SULPHIDE VEINS, AND ALSO A DENSE STOCKWORK NETWORK OF VEINLETS. THESE ORE BODIES ARE CONFINED TO BREAKAWAY JOINTS AND TO SECTORS WHERE THEY MERGE WITH NORTHEASTERLY OR NORTHWESTERLY FAULTS. A SEGREGATED MINERALIZATION HAS BEEN OBSERVED IN THE GENTLY-DIPPING MYLONITIZED ZONES IN THE MARGINAL PORTION OF THE INTRUSIVE MASSIF. --FROM SMIRNOV 1977 P. 54 VOL. III. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JUL-1990 | Paidakovich, Matthew E. | U.S. Geological Survey | |
| Updater | 01-FEB-1994 | Jenness, Jane E. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.