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FAULT-RELATED DOLOMITIZATION WITH HYDROTHERMAL WALL-ROCK ALTERATION IN KINTA VALLEY, PERAK, MALAYSIA.

Thick Devonian-Permian carbonates were deposited on a shallow marine before being uplifted by granitic intrusion during Triassic. These dolomite bodies are commonly found in Kinta Limestone. After the granite intrusion near the Kinta Valley, the residual fluid rose upward through the structure forme...

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Main Author: MOHAMMAD ZAHIR, NURUL AFIQAH
Format: Thesis
Language:English
Published: 2020
Subjects:
QE Geology
Online Access:http://utpedia.utp.edu.my/20563/1/Nurul%20Afiqah_16004001.pdf
http://utpedia.utp.edu.my/20563/
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spelling my-utp-utpedia.205632021-08-30T16:28:33Z http://utpedia.utp.edu.my/20563/ FAULT-RELATED DOLOMITIZATION WITH HYDROTHERMAL WALL-ROCK ALTERATION IN KINTA VALLEY, PERAK, MALAYSIA. MOHAMMAD ZAHIR, NURUL AFIQAH QE Geology Thick Devonian-Permian carbonates were deposited on a shallow marine before being uplifted by granitic intrusion during Triassic. These dolomite bodies are commonly found in Kinta Limestone. After the granite intrusion near the Kinta Valley, the residual fluid rose upward through the structure formed especially in deep-seated faults. The existing structures that are present in the host rocks that might controlled the hydrothermal dolomite formation have never been investigated in detail. Besides, dolomite formed in the Kinta Valley was found to be massive and there was a possibility of hydrothermal dolomitization attacked on the host rock which altered it into dolomite. 2020-10 Thesis NonPeerReviewed application/pdf en http://utpedia.utp.edu.my/20563/1/Nurul%20Afiqah_16004001.pdf MOHAMMAD ZAHIR, NURUL AFIQAH (2020) FAULT-RELATED DOLOMITIZATION WITH HYDROTHERMAL WALL-ROCK ALTERATION IN KINTA VALLEY, PERAK, MALAYSIA. Masters thesis, Universiti Teknologi PETRONAS.
institution Universiti Teknologi Petronas
building UTP Resource Centre
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Teknologi Petronas
content_source UTP Electronic and Digitized Intellectual Asset
url_provider http://utpedia.utp.edu.my/
language English
topic QE Geology
spellingShingle QE Geology
MOHAMMAD ZAHIR, NURUL AFIQAH
FAULT-RELATED DOLOMITIZATION WITH HYDROTHERMAL WALL-ROCK ALTERATION IN KINTA VALLEY, PERAK, MALAYSIA.
description Thick Devonian-Permian carbonates were deposited on a shallow marine before being uplifted by granitic intrusion during Triassic. These dolomite bodies are commonly found in Kinta Limestone. After the granite intrusion near the Kinta Valley, the residual fluid rose upward through the structure formed especially in deep-seated faults. The existing structures that are present in the host rocks that might controlled the hydrothermal dolomite formation have never been investigated in detail. Besides, dolomite formed in the Kinta Valley was found to be massive and there was a possibility of hydrothermal dolomitization attacked on the host rock which altered it into dolomite.
format Thesis
author MOHAMMAD ZAHIR, NURUL AFIQAH
author_facet MOHAMMAD ZAHIR, NURUL AFIQAH
author_sort MOHAMMAD ZAHIR, NURUL AFIQAH
title FAULT-RELATED DOLOMITIZATION WITH HYDROTHERMAL WALL-ROCK ALTERATION IN KINTA VALLEY, PERAK, MALAYSIA.
title_short FAULT-RELATED DOLOMITIZATION WITH HYDROTHERMAL WALL-ROCK ALTERATION IN KINTA VALLEY, PERAK, MALAYSIA.
title_full FAULT-RELATED DOLOMITIZATION WITH HYDROTHERMAL WALL-ROCK ALTERATION IN KINTA VALLEY, PERAK, MALAYSIA.
title_fullStr FAULT-RELATED DOLOMITIZATION WITH HYDROTHERMAL WALL-ROCK ALTERATION IN KINTA VALLEY, PERAK, MALAYSIA.
title_full_unstemmed FAULT-RELATED DOLOMITIZATION WITH HYDROTHERMAL WALL-ROCK ALTERATION IN KINTA VALLEY, PERAK, MALAYSIA.
title_sort fault-related dolomitization with hydrothermal wall-rock alteration in kinta valley, perak, malaysia.
publishDate 2020
url http://utpedia.utp.edu.my/20563/1/Nurul%20Afiqah_16004001.pdf
http://utpedia.utp.edu.my/20563/
_version_ 1739832769563852800
score 13.15806

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