Transport and deposition of cassiterite by a Malaysian stream W. K. Fletcher, C. H. Loh.
Material type:
TextPublisher: 1997Description: 6p. ill. 27cmSubject(s): Geology, Economic -- Malacca | Rocks, Igneous -- Malacca | Sedimentation and deposition -- Malacca | Cassiterite -- Malacca | Sediments (Geology) -- Malacca | Gold -- Malacca | Gunung Bujang (Malacca)Summary: Low abundances of @heavy@ heavy minerals, such as cassiterite and gold, in natural sediments make it difficult to observe and monitor the sedimentological processes that lead to the development of their placer deposits in fluvial channels. We have overcome this problem by installation of apit trap in a Malaysian stream that contains abnormally high concentrations of cassiterite. Rates of accumulation of cassiterite grains up to 500 mm and sediment up to 30 mm have been measured under changing discharges during a flood event.
| Item type | Current location | Collection | Call number | Status | Date due | Barcode | Item holds |
|---|---|---|---|---|---|---|---|
| Reports | JMG IBUPEJABAT Open Shelf | Open Shelf | 549.52409595 FLE (Browse shelf) | Available | 00003192 |
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| 549.52309595122 JPW Prospecting report on Terengganu ilmenite | 549.524 SER Notes on Lahat Pipe | 549.524 SER Notes on Lahat Pipe | 549.52409595 FLE Transport and deposition of cassiterite by a Malaysian stream | 549.5240959511242 TEO A report on the investigation of cassiterite/ wolframite bearing quartz veins in Song Kee Tin Mine, Kulim | 549.52409595115 ROE Report on wolfram cassiterite lodes near Ulu Yam, Selangor | 549.52409595119 HIL Cassiterite mineralization and its relation to wall rock alteration |
Journal of Sedimentary Research, Vol.67, No.5, September, 1997, 763-775.
Low abundances of @heavy@ heavy minerals, such as cassiterite and gold, in natural sediments make it difficult to observe and monitor the sedimentological processes that lead to the development of their placer deposits in fluvial channels. We have overcome this problem by installation of apit trap in a Malaysian stream that contains abnormally high concentrations of cassiterite. Rates of accumulation of cassiterite grains up to 500 mm and sediment up to 30 mm have been measured under changing discharges during a flood event.
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