Geology and mineral resources of the Sungai Tekai area Pahang Darul Makmur map report 18 Khoo Han Peng

By: Khoo, Han PengMaterial type: TextTextPublisher: Kuala Lumpur Jabatan Mineral dan Geosains Malaysia 2009Description: xvii, 106p. ill., maps 30cm+ 1 mapISBN: 9789834439613Subject(s): Mineral resources -- Sg. Tekai -- PahangSummary: The Sungai Tekai area is underlain predominantly by a group of continental sediments. Only Bangak metasediments and Lempah Granite occur to the northeast. These continental sediments previously included in the Tembeling formation by B.N Koopmans in 1968 are now shown to be mappable as four lithostratigraphic units named as the Kerum Formation, Lanis Conglomerate, manghing Sandstone and Termus Shale
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Includes bibliographical references

The Sungai Tekai area is underlain predominantly by a group of continental sediments. Only Bangak metasediments and Lempah Granite occur to the northeast. These continental sediments previously included in the Tembeling formation by B.N Koopmans in 1968 are now shown to be mappable as four lithostratigraphic units named as the Kerum Formation, Lanis Conglomerate, manghing Sandstone and Termus Shale

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