Geology and petrography of granite in Pulau Redang, Terengganu

The study area is located at the Pulau Redang that is lying close to the equator, which is in the South China Sea off the northeast coast of Peninsular Malaysia. It is located about 45km north-northeast of Kuala Terengganu. The gateway to Pulau Redang, with the closest point from the mainland, is ab...

Full description

Saved in:
Bibliographic Details
Main Author: Nur Intan Syazwani Rustami
Format: Undergraduate Final Project Report
Published: 2017
Online Access:http://discol.umk.edu.my/id/eprint/7160/
Tags: Add Tag
No Tags, Be the first to tag this record!
id my.umk.eprints.7160
record_format eprints
spelling my.umk.eprints.71602022-05-23T08:51:30Z http://discol.umk.edu.my/id/eprint/7160/ Geology and petrography of granite in Pulau Redang, Terengganu Nur Intan Syazwani Rustami The study area is located at the Pulau Redang that is lying close to the equator, which is in the South China Sea off the northeast coast of Peninsular Malaysia. It is located about 45km north-northeast of Kuala Terengganu. The gateway to Pulau Redang, with the closest point from the mainland, is about 22km away from Tanjung Merang. Pulau Redang is composed with two main types of lithology. They are metasandstone and granite that can divide into two crystal sizes which are coarse crystal (granite porphyry) with grey colour and fine crystal (equigranular granite) with pink colour. It is seems that metasandstones are the older rock compared to granite rock. The age of the metasandstone is Permian and more specifically, the plutonic activities existed in the Pulau Redang at Permian to early Triassic. The textural features of granite rock cast much light on the conditions under which igneous rocks consolidates from their parent magmas. They are controlled by the rate and order of crystallization, which depends in, turn on the initial temperatures. Besides, it also depends on the composition, gas content and viscosity of the magma and the pressure at which it solidifies. The main differences between granite porphyry and equigranular granite are basically based on petrographic studies. 2017 Undergraduate Final Project Report NonPeerReviewed Nur Intan Syazwani Rustami (2017) Geology and petrography of granite in Pulau Redang, Terengganu. Undergraduate Final Project Report thesis, Faculty of Earth Sciences. (Submitted)
institution Universiti Malaysia Kelantan
building Perpustakaan Universiti Malaysia Kelantan
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Malaysia Kelantan
content_source UMK Institutional Repository
url_provider http://umkeprints.umk.edu.my/
description The study area is located at the Pulau Redang that is lying close to the equator, which is in the South China Sea off the northeast coast of Peninsular Malaysia. It is located about 45km north-northeast of Kuala Terengganu. The gateway to Pulau Redang, with the closest point from the mainland, is about 22km away from Tanjung Merang. Pulau Redang is composed with two main types of lithology. They are metasandstone and granite that can divide into two crystal sizes which are coarse crystal (granite porphyry) with grey colour and fine crystal (equigranular granite) with pink colour. It is seems that metasandstones are the older rock compared to granite rock. The age of the metasandstone is Permian and more specifically, the plutonic activities existed in the Pulau Redang at Permian to early Triassic. The textural features of granite rock cast much light on the conditions under which igneous rocks consolidates from their parent magmas. They are controlled by the rate and order of crystallization, which depends in, turn on the initial temperatures. Besides, it also depends on the composition, gas content and viscosity of the magma and the pressure at which it solidifies. The main differences between granite porphyry and equigranular granite are basically based on petrographic studies.
format Undergraduate Final Project Report
author Nur Intan Syazwani Rustami
spellingShingle Nur Intan Syazwani Rustami
Geology and petrography of granite in Pulau Redang, Terengganu
author_facet Nur Intan Syazwani Rustami
author_sort Nur Intan Syazwani Rustami
title Geology and petrography of granite in Pulau Redang, Terengganu
title_short Geology and petrography of granite in Pulau Redang, Terengganu
title_full Geology and petrography of granite in Pulau Redang, Terengganu
title_fullStr Geology and petrography of granite in Pulau Redang, Terengganu
title_full_unstemmed Geology and petrography of granite in Pulau Redang, Terengganu
title_sort geology and petrography of granite in pulau redang, terengganu
publishDate 2017
url http://discol.umk.edu.my/id/eprint/7160/
_version_ 1763303801317490688
score 13.211869