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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my.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 |
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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 |
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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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Article |
author |
Ghani, Azman Abd Sofian-Azirun, Mohd Ramli, R. Hashim, Rosli Rahman, N.I. Zainuddin, Z.A. |
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Ghani, Azman Abd Sofian-Azirun, Mohd Ramli, R. Hashim, Rosli Rahman, N.I. Zainuddin, Z.A. |
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Ghani, Azman Abd |
title |
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_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_sort |
geochemical contrast between beroga (kuala kelawang pluton) and semenyih (kuala lumpur pluton) granites in kuala kelawang area, negeri sembilan |
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Geological Society of Malaysia |
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2008 |
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http://eprints.um.edu.my/8305/ http://www.gsm.org.my/products/702001-100482-PDF.pdf |
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