| Deposit ID | 10023401 |
|---|---|
| MRDS ID | I000302 |
| Record type | Site |
| Current site name | Acep |
| Geographic coordinates: | 28.20168, 39.46401 (WGS84) |
|---|---|
| Relative position | THE DEPOSIT IS 1 KM SE OF ISKELE KOY AND 2.4 KM NW OF KIRECLIK. IT IS LOCATED 1.2 M ABOVE THE FLOOR OF THE VALLEY. |
Political divisions (FIPS codes)
Balikesir(province)
Turkey(country)
Europe(continent)
Land(continent)
| Country | State |
|---|---|
| Turkey | Balikesir |
| Commodity | Importance |
|---|---|
| Boron-Borates | Primary |
| Materials | Type of material |
|---|---|
| Inyoite | Ore |
| Ulexite | Ore |
| Bentonite | Gangue |
| Clay | Gangue |
| Model code | 260 |
|---|---|
| USGS model code | 35b.3 |
| Deposit model name | Lacustrine borates |
| Host or associated | Associated | ||||
|---|---|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Glassy Rock > Obsidian | ||||
| |||||
| Host or associated | Associated |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite |
| Host or associated | Host |
|---|---|
| Rock type | Unconsolidated Deposit > Clay, Mud |
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Carbonate > Limestone |
| Host or associated | Host |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Pyroclastic Rock > Tuff |
| (1) | 28.20168, 39.46401 |
|---|
| Dip | NE |
|---|
| Development status | Past Producer |
|---|---|
| Commodity type | Non-metallic |
| Significant | No |
| District name | Bigadic - Iskelekoy Area |
|---|
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | I000302 |
MINERAL RESEARCH AND EXPLORATION INSTITUTE OF TURKEY, 1965, BORATE DEPOSITS OF TURKEY: MINERAL RESEARCH AND EXPLORATION INSTITUTE OF TURKEY PUBLICATION 125, 11 P
MINERAL RESEARCH AND EXPLORATION INSTITUTE OF TURKEY, 1965.
| Subject category | Comment text |
|---|---|
| Deposit | THE DEPOSIT CONSISTS OF ULEXITE WITH A THIN ZONE OF COLEMANITE NEAR THE FLOOR. THE DEPOSIT IS LOCATED ALONG THE SAME STRIKE DIRECTION AS THE KURTPINARI-GUNEVI-BEGENDIKLER DEPOSITS. THE ORE-BEARING LAYER IS ALMOST 3 M THICK BUT CONTAINS MORE CLAY PARTINS THAN THE DEPOSITS TO THE NORTH. A COLEMANITE ZONE IS SUSPECTED, BUT NO EXPLORATION WORK HAD BEEN DONE TO CONFIRM THIS. BENTONITIC MATERIAL IS FOUND AS FLOOR GOUGE. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-FEB-1990 | Orris, Greta J. | U.S. Geological Survey | |
| Updater | 01-OCT-1993 | Orris, Greta J. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.