Geochemical contrast between Beroga (Kuala Kelawang pluton) and Semenyih (Kuala Lumpur pluton) granites in Kuala Kelawang area, Negeri Sembilan

Geochemical data of both Semenyih and Beroga granites, in the central part of Main Range Granite, show that they are madeup of different magma pulses. The Beroga granite is more basic, containing 67.22 - 68.02% SiO2, whereas the Semenyih granite consists of more evolved rock (SiO2 : 70.36 to 73.48%)...

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Main Authors: Ghani, Azman Abd, Sofian-Azirun, Mohd, Ramli, R., Hashim, Rosli, Rahman, N.I., Zainuddin, Z.A.
Format: Article
Published: Geological Society of Malaysia 2008
Subjects:
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author Ghani, Azman Abd
Sofian-Azirun, Mohd
Ramli, R.
Hashim, Rosli
Rahman, N.I.
Zainuddin, Z.A.
author_facet Ghani, Azman Abd
Sofian-Azirun, Mohd
Ramli, R.
Hashim, Rosli
Rahman, N.I.
Zainuddin, Z.A.
author_sort Ghani, Azman Abd
collection UM
description Geochemical data of both Semenyih and Beroga granites, in the central part of Main Range Granite, show that they are madeup of different magma pulses. The Beroga granite is more basic, containing 67.22 - 68.02% SiO2, whereas the Semenyih granite consists of more evolved rock (SiO2 : 70.36 to 73.48%). Both are S-type granite which suggests that the source rocks were metasediments. Geochemically, they are part of the Main Range Granite. The Semenyih granite is charcterised by high Rb/Sr ratio, which suggests that the magma is highly evolved and contains less enclaves compared to the Beroga granite.
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spelling um.eprints-83052019-05-31T05:34:50Z http://eprints.um.edu.my/8305/ Geochemical contrast between Beroga (Kuala Kelawang pluton) and Semenyih (Kuala Lumpur pluton) granites in Kuala Kelawang area, Negeri Sembilan Ghani, Azman Abd Sofian-Azirun, Mohd Ramli, R. Hashim, Rosli Rahman, N.I. Zainuddin, Z.A. QH301 Biology Geochemical data of both Semenyih and Beroga granites, in the central part of Main Range Granite, show that they are madeup of different magma pulses. The Beroga granite is more basic, containing 67.22 - 68.02% SiO2, whereas the Semenyih granite consists of more evolved rock (SiO2 : 70.36 to 73.48%). Both are S-type granite which suggests that the source rocks were metasediments. Geochemically, they are part of the Main Range Granite. The Semenyih granite is charcterised by high Rb/Sr ratio, which suggests that the magma is highly evolved and contains less enclaves compared to the Beroga granite. Geological Society of Malaysia 2008 Article PeerReviewed Ghani, Azman Abd and Sofian-Azirun, Mohd and Ramli, R. and Hashim, Rosli and Rahman, N.I. and Zainuddin, Z.A. (2008) Geochemical contrast between Beroga (Kuala Kelawang pluton) and Semenyih (Kuala Lumpur pluton) granites in Kuala Kelawang area, Negeri Sembilan. Bulletin of the Geological Society of Malaysia, 54. pp. 71-74. ISSN 0126-6187, http://www.gsm.org.my/products/702001-100482-PDF.pdf
spellingShingle QH301 Biology
Ghani, Azman Abd
Sofian-Azirun, Mohd
Ramli, R.
Hashim, Rosli
Rahman, N.I.
Zainuddin, Z.A.
Geochemical contrast between Beroga (Kuala Kelawang pluton) and Semenyih (Kuala Lumpur pluton) granites in Kuala Kelawang area, Negeri Sembilan
title Geochemical contrast between Beroga (Kuala Kelawang pluton) and Semenyih (Kuala Lumpur pluton) granites in Kuala Kelawang area, Negeri Sembilan
title_full Geochemical contrast between Beroga (Kuala Kelawang pluton) and Semenyih (Kuala Lumpur pluton) granites in Kuala Kelawang area, Negeri Sembilan
title_fullStr Geochemical contrast between Beroga (Kuala Kelawang pluton) and Semenyih (Kuala Lumpur pluton) granites in Kuala Kelawang area, Negeri Sembilan
title_full_unstemmed Geochemical contrast between Beroga (Kuala Kelawang pluton) and Semenyih (Kuala Lumpur pluton) granites in Kuala Kelawang area, Negeri Sembilan
title_short Geochemical contrast between Beroga (Kuala Kelawang pluton) and Semenyih (Kuala Lumpur pluton) granites in Kuala Kelawang area, Negeri Sembilan
title_sort geochemical contrast between beroga kuala kelawang pluton and semenyih kuala lumpur pluton granites in kuala kelawang area negeri sembilan
topic QH301 Biology
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