| Deposit ID | 10023523 |
|---|---|
| MRDS ID | I000609 |
| Record type | Site |
| Current site name | Shawei |
| Alternate or previous names | Sha-Wei |
| Geographic coordinates: | 112.99948, 21.51619 (WGS84) |
|---|---|
| Location accuracy | 10000(meters) |
| Relative position | Estimated Location, May Be 10 Minutes Off., Estimated Location, May Be 10 Minutes Off. |
Political divisions (FIPS codes)
Guangdong [Kwangtung](province)
China(country)
Asia(continent)
Land(continent)
| Country | State |
|---|---|
| China | Guangdong [Kwangtung] |
| Commodity | Importance |
|---|---|
| Kaolin | Primary |
| Materials | Type of material |
|---|---|
| Kaolin | Ore |
| Feldspar | Gangue |
| Gibbsite | Gangue |
| Halloysite | Gangue |
| Illite | Gangue |
| Quartz | Gangue |
| Result | KAOLIN GENERALLY HAS < 0.02% TIO2 |
|---|---|
| Result | <1% FE2O3 |
| Result | SIO2/AL2O3 RATIO OF 2.2 TO 2.5 |
| Result | LOW CONTENTS OF NA, CA, MG, AND MN. MAIN ORES HAVE 67-70% SIO2 AND 20-23% AL2O3 |
| Result | AFTER SIEVING AT 320 MESH, THE SIO2 CONTENT IS 47-50% AND AL2O3 IS 33-36%. |
| Host or associated | Associated |
|---|---|
| Rock type | Plutonic Rock > Granitoid > Monzonite |
| Host or associated | Host |
|---|---|
| Rock type | Plutonic Rock > Granitoid > Monzonite |
| (1) | 112.99948, 21.51619 |
|---|
| Development status | Producer |
|---|---|
| Commodity type | Non-metallic |
| Significant | No |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | I000609 |
GUOPING, ZHOU, 1990, A STUDY OF WEATHERING CRUST KAOLIN DEPOSIT IN GUANGDONG PROVINCE: MINERAL DEPOSITS, V. 9, NO. 2, P. 174-175
| Subject category | Comment text |
|---|---|
| Deposit | KAOLIN DEPOSIT HAS STYLES OF MINERALIZATION, DETERMINABLE BY ASSOCIATED RARE EARTH MINERALS. THE FIRST IS AN ALBITIZED KAOLIN FORMED FROM MUSCOVITE MONZONITIC GRANITE; THE SECOND AN ALBITIZED KAOLIN FORMED FROM A PORPHYRITIC 2-MICA MONZONITIC GRANITE. THE ORES CONSIST OF KAOLIN WITH HALLOYSITE, ILLITE, QUARTZ, AND MINOR FELDSPAR. THE V4 OREBODY IS 70-85% KAOLINITE AND 9-20% ILLITE. THE V2 OREBODY IS 50-82% KAOLINITE AND 12-27% ILLITE. HALLOYSITE IS WELL DEVELOPED IN THE MIDDLE OF THE OREBODY AND A SMALL AMOUNT OF GIBBSITE OCCURS NEAR THE UPPER PART OF THE DEPOSIT AS A RESULT OF THE WEATHERING (DEHYDRATION AT SURFACE). |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-OCT-90 | Orris, Greta J. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.