| Deposit ID | 10066756 |
|---|---|
| MRDS ID | TC43054 |
| Record type | Site |
| Current site name | The Granites |
| Geographic coordinates: | 130.3324, -20.58003 (WGS84) |
|---|---|
| Location accuracy | 1000(meters) |
| Relative position | 550 KM W OF ALICE SPRINGS., Estiamted Location. |
Political divisions (FIPS codes)
Northern Territory*(province)
Australia(country)
Australia(continent)
Land(continent)
| Country | State |
|---|---|
| Australia | Northern Territory* |
| Commodity | Importance |
|---|---|
| Gold | Primary |
| Materials | Type of material |
|---|---|
| Gold | Ore |
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Sedimentary Rock > Chemical Sediment > Iron Formation | ||
| |||
| (1) | 130.3324, -20.58003 |
|---|
| Development status | Producer |
|---|---|
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | No |
| Discovery year | 1900 |
| Type | Owner |
|---|---|
| Owner | Posgold (Division Of Normandy Poseidon, |
| Last year | 1993 |
| Type | In-situ | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Estimate year | 1990 | ||||||||||||||
| Total resources | 2320000000mt ore | ||||||||||||||
| |||||||||||||||
| Type | In-situ | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Estimate year | 1993 | ||||||||||||||
| Total resources | 1000000000mt ore | ||||||||||||||
| |||||||||||||||
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | TC43054 |
SOLOMON, M., AND GROVES, D.I., 1994, THE GEOLOGY AND ORIGIN OF AUSTRALIA'S MINERAL DEPOSITS: OXFORD, OXFORD MONOGRAPHS ON GEOLOGY AND GEOPHYSICS 24, 951 P.
ENGINEERING AND MINING JOURNAL, JUNE, 1987.
STEWART, NEIL, 1993, AUSTRALIA: MINING ANNUAL REVIEW--1993, P. 135-142.
STEWART, G.N., 1991, AUSTRALIA: MINING ANNUAL REVIEW--1991, P. 69-78.
STEWART, 1993; STEWART, 1991.
SOLOMON AND GROVES, 1994; STEWART, 1991; STEWART, 1993.
| Subject category | Comment text |
|---|---|
| Deposit | AU IS HOSTED BY SILICATE, SILICATE-SULFIDE, CARBONATE, AND OXIDE FACIES OF BANDED IRON FORMATION. THE SEQUENCE IS METAMORPHOSED TO HORNFELS FACIES AND SUBSEQUENTLY RETROGRESSED. THE AU MINERALIZATION APPEARS TO HAVE BEEN BOTH EARLY AND LATE IN DEFORMATION HISTORY AND MAY BE RELATED TO REGIONAL METAMORPHISM AND EARLY GRANITE MAGMATISM. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-APR-95 | Orris, Greta J. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.