Sungei Besi Mines Ltd., Selangor a magnetic traverse along the eastern side of the Old Hong Fatt Mine J. H. Hill.
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TextPublisher: 1963Description: 4p. 33cmSubject(s): Geology -- Selangor -- Sungei Besi | Mineralogy -- Selangor -- Sungei Besi | Sungei Besi (Selangor)Summary: Limestones overlain by Quaternary sediments are exposed along the western side of the pit while granite and granite wash are exposed on the eastern side. The contact between granite and limestone trends approximately north-south along the centre of the pit. Intrusive into granitic rocks are cassiterite-bearing veins, of variable width, striking in an easterly direction with which magnetite was thought to be associated. This mineralisation can frequently be traced along the strike by a line of ironstained float. Also striking in an easterly direction across the granite ore white quartz veins.
| Item type | Current location | Collection | Call number | Status | Date due | Barcode | Item holds |
|---|---|---|---|---|---|---|---|
| Reports | JMG IBUPEJABAT Open Shelf | Open Shelf | 555.95115 HIL (Browse shelf) | Available | 00003274 |
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Limestones overlain by Quaternary sediments are exposed along the western side of the pit while granite and granite wash are exposed on the eastern side. The contact between granite and limestone trends approximately north-south along the centre of the pit. Intrusive into granitic rocks are cassiterite-bearing veins, of variable width, striking in an easterly direction with which magnetite was thought to be associated. This mineralisation can frequently be traced along the strike by a line of ironstained float. Also striking in an easterly direction across the granite ore white quartz veins.
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