Potential for primary tin mineralization and an account of the tin mining activities of the Klian Intan area, Upper Perak Khoo Kay Khean
Material type:
TextPublisher: 1982Description: 75p. col., ill., maps 31cmSubject(s): Mineralogy -- Perak -- Klian Intan | Geology, Economic -- Perak -- Klian Intan | Tin mines and mining -- Perak -- Klian Intan | Klian Intan (Perak) | Sungei Pong (Perak) | Sungei Pahit (Perak)Summary: The Klian Intan area is underlain by rocks of the Baling Formation consisting of quartzites, argillites, hornfelses and marble of Lower Silurian and older age. Exposures seen at the Rahman Hydraulic Tin Limited mine at Gunung Paku show that the mineralization there can be attributed to a stock work type deposit characterised by numerous cassiterite-quartz-polymetallic sulphide veins and lodes crian-crossing the country rocks.
| Item type | Current location | Collection | Call number | Status | Date due | Barcode | Item holds |
|---|---|---|---|---|---|---|---|
| Reports | JMG IBUPEJABAT Open Shelf | Open Shelf | 549.09595114 KHO (Browse shelf) | Available | 00003188 |
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August, 1982
The Klian Intan area is underlain by rocks of the Baling Formation consisting of quartzites, argillites, hornfelses and marble of Lower Silurian and older age. Exposures seen at the Rahman Hydraulic Tin Limited mine at Gunung Paku show that the mineralization there can be attributed to a stock work type deposit characterised by numerous cassiterite-quartz-polymetallic sulphide veins and lodes crian-crossing the country rocks.
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