General geology of Batu Kawa/Tundong/Lundu road area Ling Nan Ley

By: Ling, Nan LeyMaterial type: TextTextPublisher: 1994Description: 1v. (unnumbered) ill., map 30 cmSubject(s): Geology -- Sarawak -- Lundu | Limestone -- Sarawak -- Lundu | Sandstone -- Sarawak -- Lundu | Geology, Stratigraphic -- Sarawak -- Lundu | Lundu (Sarawak)Summary: The general geology of Batu Kawa/Tundong Road Area is depicted in the figure attached.The rock of Pedawan Formation which are of the Late Jurassic to late Creataceous age are the oklest rock in the area. In formation consist of a thick sequence of moderately to steeply-dipping marine sedimentary rock,predominantle shale and mudstone with subordinate sandstone and lenses of fossiliferous limestone
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The general geology of Batu Kawa/Tundong Road Area is depicted in the figure attached.The rock of Pedawan Formation which are of the Late Jurassic to late Creataceous age are the oklest rock in the area. In formation consist of a thick sequence of moderately to steeply-dipping marine sedimentary rock,predominantle shale and mudstone with subordinate sandstone and lenses of fossiliferous limestone

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