| Deposit ID | 10067122 |
|---|---|
| MRDS ID | TC50311 |
| Record type | Site |
| Current site name | Gallito |
| Alternate or previous names | Mina Gallito |
| Geographic coordinates: | -62.90635, 6.01794 (WGS84) |
|---|
Political divisions (FIPS codes)
Bolivar(province)
Venezuela(country)
South America(continent)
Land(continent)
| Country | State |
|---|---|
| Venezuela | Bolivar |
| Commodity | Importance |
|---|---|
| Diamond | Primary |
| Materials | Type of material |
|---|---|
| Diamond | Ore |
| Gibbsite | Gangue |
| Kaolin | Gangue |
| Muscovite | Gangue |
| Quartz | Gangue |
| Model code | 122 |
|---|---|
| USGS model code | 39d |
| Deposit model name | Diamond placer |
| Host or associated | Associated | ||
|---|---|---|---|
| Rock type | Plutonic Rock > Mafic Intrusive Rock > Diorite > Diabase | ||
| |||
| Host or associated | Host |
|---|---|
| Rock type | Unconsolidated Deposit > Gravel |
| Rock unit name | Pre-Roraima Formation |
| Rock description | Pre-Roraima Formation |
| (1) | -62.90635, 6.01794 |
|---|
| Development status | Producer |
|---|---|
| Commodity type | Non-metallic |
| Deposit size | Small |
| Significant | No |
| District name | San Salvador De Paul |
|---|
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | TC50311 |
BRICENO, H.O., 1982, APPLICATION OF REMOTE SENSING TO DIAMOND PLACER EXPLORATION IN A TROPICAL JUNGLE ENVIRONMENT, CARONI RIVER, VENEZUELA: GOLDEN, COLORADO, COLORADO SCHOOL OF MINES, PH.D. DISSERTATION.
BRICENO M., H.O., 1985, GENESIS DE YACIMIENTOS MINERALES VENEZOLANOS II: PLACERES DIAMANTIFEROS DE SAN SALVADOR DE PAUL: ACTA CIENTIFICA VENEZOLANA, V. 36, P. 154-158.
CIMRI
BRICENO, 1982
| Subject category | Comment text |
|---|---|
| Deposit | DIAMOND BEARING GRAVELS FORM 2 THIN UNITS. LOWER GRAVEL (DARK ORE) IS 5-10 CM THICK AND CONTAINS IRON CONCRETIONS, SILICIFIED SANDSTONE FRAGMENTS, VEIN QUARTZ FRAGMENTS, AND CLAY. THE UPPER GRAVEL CONTAINS VEIN QUARTZ, SILICIFIED SANDSTONE FRAGMENTS AND CLAY MATERIAL, BUT HAS NO IRON CONCRETIONS. NO KIMBERLITIC MATERIAL HAS BEEN FOUND IN THE GRAVELS. THE LOWER GRAVEL IS MIXED WITH ORGANIC MATERIAL. NO KIMBERLITIC MATERIAL HAS BEEN FOUND IN THIS AREA. THE DIAMONDS IN THE YOUNG SEDIMENTS ARE BELIEVED TO BE DERIVED FROM PALEO-PLACERS IN THE PREC SEDIMENTARY ROCKS OF PRE-RORAIMA AND UAIREN FORMATIONS. BRICENO M. (1985) ALSO INDICATED THAT THE RECENT DIAMOND-BEARING SEDIMENTS WERE DEPOSITED UNDER ARID CLIMATIC CONDITIONS. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-SEP-1991 | Gray, Floyd | U.S. Geological Survey | |
| Updater | 01-OCT-1991 | Orris, Greta J. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.