Iron ore occurrences in Batang Kali estate, Selangor S. Macdonald.
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TextPublisher: 1961Description: 2p. ill. 33cmSubject(s): Iron ore -- Geology -- Selangor -- Batang Kali | Batang Kali (Selangor)Summary: At the first locality visited, the summit and northern slopes of Bukit Chendang, there are numerous pebbles and fragments of haematite in the soil. Many of these appear to be of high grade but others are highly siliceous. The country rock, phyllite, schists and tuffy schist, is of ten inpregnated by narrow veins of haematite.Quartz veining is common. Haematite pebbles are of ten tabular and brittle. The haematite occuring here has apparently been derived from narrow veins in the country rock and there appears to be insufficient to justify further prospecting.
| Item type | Current location | Collection | Call number | Status | Date due | Barcode | Item holds |
|---|---|---|---|---|---|---|---|
| Reports | JMG IBUPEJABAT Open Shelf | Open Shelf | 553.309595115 MAC (Browse shelf) | Available | 00003768 |
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| 553.309595114 CHU Iron ore- Sengat estate | 553.30959511431 WIL Notes on the occurences of lode tin - ore in the Kinta Valley | 553.309595115 BEA Iron ore on Sg. Gapi estate Selangor | 553.309595115 MAC Iron ore occurrences in Batang Kali estate, Selangor | 553.309595115 MNA Mineral perindustrian di Selangor dan Wilayah Persekutuan 1994 | 553.309595115 WIL An account of the geology and mining industries of south Selangor and Negeri Sembilan | 553.309595117 HAN Projek sumber mineral perindustrian semenanjung, sumber mineral perindustrian Negeri Sembilan/Melaka |
February, 1961
At the first locality visited, the summit and northern slopes of Bukit Chendang, there are numerous pebbles and fragments of haematite in the soil. Many of these appear to be of high grade but others are highly siliceous. The country rock, phyllite, schists and tuffy schist, is of ten inpregnated by narrow veins of haematite.Quartz veining is common. Haematite pebbles are of ten tabular and brittle. The haematite occuring here has apparently been derived from narrow veins in the country rock and there appears to be insufficient to justify further prospecting.
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