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:
QE Geology
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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spelling utp-eprints.122302017-06-05T08:07:07Z Geological Structures of the Kinta Valley Revisited Using Drainage Anomalies Choong Chee Meng, Manuel Pubellier, . QE Geology 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 severely deformed. Unfortunately, these rocks are restricted to small areas of the valley and they are highly weathered, thus making the correlations between outcrops and structural interpretation commonly speculative. 2015 Article PeerReviewed https://link.springer.com/chapter/10.1007/978-981-287-368-2_25 Choong Chee Meng, Manuel Pubellier, . (2015) Geological Structures of the Kinta Valley Revisited Using Drainage Anomalies. Geological Structures of the Kinta Valley Revisited Using Drainage Anomalies . http://eprints.utp.edu.my/12230/
institution Universiti Teknologi Petronas
collection UTP Institutional Repository
topic QE Geology
spellingShingle QE Geology
Choong Chee Meng, Manuel Pubellier, .
Geological Structures of the Kinta Valley Revisited Using Drainage Anomalies
description 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 severely deformed. Unfortunately, these rocks are restricted to small areas of the valley and they are highly weathered, thus making the correlations between outcrops and structural interpretation commonly speculative.
format Article
author Choong Chee Meng, Manuel Pubellier, .
author_sort Choong Chee Meng, Manuel Pubellier, .
title Geological Structures of the Kinta Valley Revisited Using Drainage Anomalies
title_short Geological Structures of the Kinta Valley Revisited Using Drainage Anomalies
title_full Geological Structures of the Kinta Valley Revisited Using Drainage Anomalies
title_fullStr Geological Structures of the Kinta Valley Revisited Using Drainage Anomalies
title_full_unstemmed Geological Structures of the Kinta Valley Revisited Using Drainage Anomalies
title_sort geological structures of the kinta valley revisited using drainage anomalies
publishDate 2015
url https://link.springer.com/chapter/10.1007/978-981-287-368-2_25
http://eprints.utp.edu.my/12230/
_version_ 1741196158842175488
score 11.62408

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