Geological Structures of the Kinta Valley Revisited Using Drainage Anomalies
ore than 50% of the surface of Kinta Valley is covered by alluvium overlying Paleozoic sequences and Late Triassic granitic intrusions. The alluvium of the valley is thin (mostly less than 30 m thick). Limestone and shale are the dominant lithologies cropping out in the valley, and they have been...
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| Format: | Article |
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2015
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| Online Access: | https://link.springer.com/chapter/10.1007/978-981-287-368-2_25 http://eprints.utp.edu.my/12230/ |
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