KLEDANG FAULT: A STRIKE-SLIP FAULT?

Kledang Fault is located in the eastern foothill of the Kledang Range in Kinta Valley which has been classified as dip-slip fault by Gobbett (1971). This fault has been clearly observed at regional-scale due to its linear feature and length (> 35km). In our recent outcrop-scale observation, ev...

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Main Author: Choong Chee Meng, Askury Abd Kadir, Siti Nur Fathiyah Jamaludin, .
Format: Article
Institution: Universiti Teknologi Petronas
Record Id / ISBN-0: utp-eprints.12234 /
Published: 2015
Subjects:
QE Geology
Online Access: http://geology.um.edu.my/gsmpublic/NGC2015/Program%20Book/Raw/Hall%20A/Hall%20A/A09_%20Choong%20Chee%20Meng_UTP.pdf
http://eprints.utp.edu.my/12234/
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spelling utp-eprints.122342017-06-05T08:08:39Z KLEDANG FAULT: A STRIKE-SLIP FAULT? Choong Chee Meng, Askury Abd Kadir, Siti Nur Fathiyah Jamaludin, . QE Geology Kledang Fault is located in the eastern foothill of the Kledang Range in Kinta Valley which has been classified as dip-slip fault by Gobbett (1971). This fault has been clearly observed at regional-scale due to its linear feature and length (> 35km). In our recent outcrop-scale observation, evidences for consistent right-lateral strike-slip fault sets were found along the foothill of southern Kledang Range where they are very close to the location of the Kledang Fault. 2015 Article PeerReviewed http://geology.um.edu.my/gsmpublic/NGC2015/Program%20Book/Raw/Hall%20A/Hall%20A/A09_%20Choong%20Chee%20Meng_UTP.pdf Choong Chee Meng, Askury Abd Kadir, Siti Nur Fathiyah Jamaludin, . (2015) KLEDANG FAULT: A STRIKE-SLIP FAULT? KLEDANG FAULT: A STRIKE-SLIP FAULT? . http://eprints.utp.edu.my/12234/
institution Universiti Teknologi Petronas
collection UTP Institutional Repository
topic QE Geology
spellingShingle QE Geology
Choong Chee Meng, Askury Abd Kadir, Siti Nur Fathiyah Jamaludin, .
KLEDANG FAULT: A STRIKE-SLIP FAULT?
description Kledang Fault is located in the eastern foothill of the Kledang Range in Kinta Valley which has been classified as dip-slip fault by Gobbett (1971). This fault has been clearly observed at regional-scale due to its linear feature and length (> 35km). In our recent outcrop-scale observation, evidences for consistent right-lateral strike-slip fault sets were found along the foothill of southern Kledang Range where they are very close to the location of the Kledang Fault.
format Article
author Choong Chee Meng, Askury Abd Kadir, Siti Nur Fathiyah Jamaludin, .
author_sort Choong Chee Meng, Askury Abd Kadir, Siti Nur Fathiyah Jamaludin, .
title KLEDANG FAULT: A STRIKE-SLIP FAULT?
title_short KLEDANG FAULT: A STRIKE-SLIP FAULT?
title_full KLEDANG FAULT: A STRIKE-SLIP FAULT?
title_fullStr KLEDANG FAULT: A STRIKE-SLIP FAULT?
title_full_unstemmed KLEDANG FAULT: A STRIKE-SLIP FAULT?
title_sort kledang fault: a strike-slip fault?
publishDate 2015
url http://geology.um.edu.my/gsmpublic/NGC2015/Program%20Book/Raw/Hall%20A/Hall%20A/A09_%20Choong%20Chee%20Meng_UTP.pdf
http://eprints.utp.edu.my/12234/
_version_ 1741196159477612544
score 11.62408

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