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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Main Author: Choong Chee Meng, Manuel Pubellier, .
Format: Article
Institution: Universiti Teknologi Petronas
Record Id / ISBN-0: utp-eprints.12230 /
Published: 2015
Subjects:
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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