Quaternary geology of the Limbang area, Sarawak Ab. Rashid Ahmad

By: Ab. Rashid AhmadMaterial type: TextTextPublisher: 1996Description: 131p. ill., maps, col. photos 30 cmSubject(s): Geology -- Sarawak -- Limbang | Geology, Stratigraphic -- Quaternary -- Sarawak -- Limbang | Limbang (Sarawak)Summary: The Limbang area is situated in the north west Sarawak bordered in the east and west bye the State of Brunei. In term of tectonic province the Limbang area was Formed in the Neogene Peripheral Basin (R,M.Banda,1996). The Quartenary geology of the area was closely related to the sea level change in the Pleistocene ang Holocene time.
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The Limbang area is situated in the north west Sarawak bordered in the east and west bye the State of Brunei. In term of tectonic province the Limbang area was Formed in the Neogene Peripheral Basin (R,M.Banda,1996). The Quartenary geology of the area was closely related to the sea level change in the Pleistocene ang Holocene time.

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