| Deposit ID | 10023405 |
|---|---|
| MRDS ID | I000306 |
| Record type | Site |
| Current site name | Kireclik |
| Alternate or previous names | Buyuk Kireclik, Kucuk Kireclik |
| Geographic coordinates: | 28.24335, 39.45429 (WGS84) |
|---|---|
| Relative position | THIS DEPOSIT IS 1.5 KM S OF KURTPINARI. |
Political divisions (FIPS codes)
Balikesir(province)
Turkey(country)
Europe(continent)
Land(continent)
| Country | State |
|---|---|
| Turkey | Balikesir |
| Commodity | Importance |
|---|---|
| Boron-Borates | Primary |
| Bentonite | Tertiary |
| Materials | Type of material |
|---|---|
| Colemanite | 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) | 28.24335, 39.45429 |
|---|
| Thickness | 3M |
|---|
| Development status | Past Producer |
|---|---|
| Commodity type | Non-metallic |
| Significant | No |
| District name | Bigadic - Iskelekoy Area |
|---|
| Type | Owner |
|---|---|
| Owner | Yakal Borasit Ltd. |
| First year | 1965 |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | I000306 |
MINERAL RESEARCH AND EXPLORATION INSTITUTE OF TURKEY, 1965, BORATE DEPOSITS OF TURKEY: MINERAL RESEARCH AND EXPLORATION INSTITUTE OF TURKEY PUBLICATION 125, 11 P
| Subject category | Comment text |
|---|---|
| Deposit | THE DEPOSIT IN BUYUK KIRECLIK INCLUDES COLEMANITE, MEYERHOFFERITE, AND PRICEITE, BUT KUCUK KIRECLIK CONTAINS ONLY COLEMANITE. AT BUYUK KIRECLIK, NODULES OF PRICEITE OCCUR WITHIN THE COLEMANITE. THE ORE-BEARING LAYER IS ABOUT 2.5-3.0 M THICK. THE ORE HAS MANY CAVITIES WITH LARGE CRYSTALS LINING THE WALLS. CLAY PARTINGS CONSTITUTE ONLY A SMALL PERCENTAGE OF THE DEPOSIT. BENTONITE IS FREQUENTLY FOUND WITHIN THE GOUGE IN THE ROOF OR FLOOR OF THE DEPOSIT AND IS CONSIDERED TO BE OF TUFFACEOUS ORIGIN. THE BENTONITE MAY BE 0.1-0.2 M THICK AND OFTEN EXHIBIT SLICKENSIDES ON THEIR SURFACES. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-FEB-1990 | Orris, Greta J. | U.S. Geological Survey | |
| Updater | 01-APR-1994 | Orris, Greta J. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.