| Deposit ID | 10023343 |
|---|---|
| MRDS ID | I000215 |
| Record type | Site |
| Current site name | Lapso Buru Mine |
| Geographic coordinates: | 85.41687, 22.83271 (WGS84) |
|---|---|
| Location accuracy | 10000(meters) |
| Relative position | DEPOSIT IS 80 KM WEST OF JAMSEDHPUR., Estimated, Believed To Be Within 10 Minutes Of True Location. |
Political divisions (FIPS codes)
Bihar(province)
India(country)
Asia(continent)
Land(continent)
| Country | State |
|---|---|
| India | Bihar |
| Commodity | Importance |
|---|---|
| Kyanite | Primary |
| Materials | Type of material |
|---|---|
| Corundum | Ore |
| Kyanite | Ore |
| Host or associated | Host | ||||
|---|---|---|---|---|---|
| Rock type | Plutonic Rock > Ultramafic Intrusive Rock > Hornblendite | ||||
| |||||
| Host or associated | Host |
|---|---|
| Rock type | Metamorphic Rock > Schist > Mica Schist |
| Host or associated | Host |
|---|---|
| Rock type | Metamorphic Rock > Granulite |
| Rock unit name | Singhbhum Iron Ore Series |
| Rock description | Singhbhum Iron Ore Series |
| (1) | 85.41687, 22.83271 |
|---|
| Type of structure | Local |
|---|---|
| Structure description | Tight Anticlines And Synclines; Singhbhum Shear Zone |
| Development status | Occurrence |
|---|---|
| Commodity type | Non-metallic |
| Significant | No |
| Discovery year | 1907 |
| Discoverer | Dr. L.L. Fermor (Identified Sample And Then Went To Describe Deposit) |
| Year of first production | 1925 |
| Type | Operator |
|---|---|
| Owner | Hindustan Copper Ltd. |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | I000215 |
MINING MAGAZINE, 1983, LAPSO BURU KYANITE: V. 149, NO. 5, P. 378-381
MINING MAGAZINE, 1983.
| Subject category | Comment text |
|---|---|
| Deposit | ORE OCCURS IN-SITU ALONG CRESTS OF RIDGE-LIKE HILLS OR AS BOULDERS BELOW THE RIDGES. THE BOULDERS MAY BE AS SMALL AS 6 MM IN DIAMETER OR AS LARGE AS SEVERAL TONNES IN WEIGHT. THE DETRITAL BOULDERS MAY BE LARGELY COMPOSED OF KYANITE OR THEY MAY BE DOMINANTLY QUARTZ OR SCHIST. THESE BOULDERS OCCUR TO A DEPTH OF 4.5 M, THE AVERAGE BEING 1.2 TO 1.5 M BELOW THE 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.