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An overview of the geology, mineralization and economic status of operating mines in the Batu Gajah sector, Perak, Malaysia Lee Ah Kow.

By: Lee, Ah KowMaterial type: Text

TextPublisher: 1991Description: v, 23p. ill., maps 30cm 1mapSubject(s): Geology -- Perak -- Batu Gajah | Geology, Economic -- Perak -- Batu Gajah | Mineralogy -- Perak -- Batu Gajah | Mines and mineral resources -- Perak -- Batu Gajah | Batu Gajah (Perak)Summary: Most (24 out of 27) of the mines are working on run-of-mine ores obtainable from stanniferous alluvium/tailings overlying the calcareous facies which is made up predominantly of marble. Ore mine borders on the geologic contacts of the calcareous and argillaceous fucies, the latter is dominated by shale, schist and phyllite. Both facies made up the devonian-carboniferous calcareous series which was metamorphosed by the post-Triassic Changkat Kantan-Tronoh-Tanjung Tualang granite. The remaining two mines are sited upon alluvium overlying the Lower Triassic Segari granite.

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Item type	Current location	Collection	Call number	Status	Date due	Item holds
Reports	JMG IBUPEJABAT Open Shelf	Open Shelf	555.95114 LEE (Browse shelf)	Available

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Previous	555.95114 BUS Lahat-Menglembu area preliminary report	555.95114 BUS Lahat-Menglembu area preliminary report	555.95114 LAP Laporan kejadian tanah mendap Taman Mewah, Kamunting, Taiping, Perak	555.95114 LEE An overview of the geology, mineralization and economic status of operating mines in the Batu Gajah sector, Perak, Malaysia	555.95114 ONG A geological investigation on the limestone hills of G. Panjang, G. Kandu, G. Mesah, G. Sepah and G. Tunggal, district of Kinta, Perak	555.95114 ONG A geological investigation on the limestone hills of G. Panjang, G. Kandu, G. Mesah, G. Sepah and G. Tunggal, district of Kinta, Perak	555.95114 SER Geological report upon Wan Yuen Mines, Menglembu, Kinta	Next

Most (24 out of 27) of the mines are working on run-of-mine ores obtainable from stanniferous alluvium/tailings overlying the calcareous facies which is made up predominantly of marble. Ore mine borders on the geologic contacts of the calcareous and argillaceous fucies, the latter is dominated by shale, schist and phyllite. Both facies made up the devonian-carboniferous calcareous series which was metamorphosed by the post-Triassic Changkat Kantan-Tronoh-Tanjung Tualang granite. The remaining two mines are sited upon alluvium overlying the Lower Triassic Segari granite.