DIAGENETIC HISTORY OF CARBONATES IN EAST SABAH
During Oligocene – Miocene, there is a major tectonic deformation which cause a widespread of uplift followed by carbonate sedimentation (Gomantong Limestone Formation) when the depositional environment changed from deep to shallow marine. These onshore Gomantong Limestone formations are often is...
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Format: | Final Year Project |
Language: | English |
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Universiti Teknologi PETRONAS
2015
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Online Access: | http://utpedia.utp.edu.my/18191/1/1.%20Dissertations%20-%20ROZEN%2015302.pdf http://utpedia.utp.edu.my/18191/ |
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