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Petrology of Northeastern Part of Gunung Jerai

bin Ash’ari, Norhalimi (2016) Petrology of Northeastern Part of Gunung Jerai. Universiti Teknologi PETRONAS. (Submitted)

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Abstract

Jerai Formation is located at the Western Belt of Peninsular Malaysia. The dominant rock type found in the study area is low grade metamorphic rock and followed by igneous rock. Quartzite is the widely observed metamorphic rocks that are formed due to the metamorphism of sandstone. Metamorphism in this area of study is believed to be initiated by contact metamorphism due to the granite plutonic intrusion under the crust. The igneous rock which is the granite are believed originated from Gunung Jerai can be interpreted to underlie the whole of Jerai Formation. Whereas pegmatite, which are the very coarse-grained, exists as intrusion or dikes associated with granitic plutons. The pegmatite formed when there is remaining magmatic fluid on the last stage of crystallization.

Item Type: Final Year Project
Academic Subject : Academic Department - Petroleum Geosciences - Petrophysics - Petrophysical data acquisition
Subject: G Geography. Anthropology. Recreation > G Geography (General)
Divisions: Geoscience and Petroleum Engineering
Depositing User: Ahmad Suhairi Mohamed Lazim
Date Deposited: 22 Nov 2018 14:39
Last Modified: 22 Nov 2018 14:39
URI: http://utpedia.utp.edu.my/id/eprint/18158

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