Late Paleogene rifting along the Malay Peninsula thickened crust
Sedimentary basins often develop above internal zones of former orogenic belts. We hereafter consider the Malay Peninsula (Western Sunda) as a crustal high separating two regions of stretched continental crust; the Andaman/Malacca basins in the western side and the Thai/Malay basins in the east....
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| Format: | Article |
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2016
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| Online Access: | http://www.sciencedirect.com/science/article/pii/S0040195116305893 http://eprints.utp.edu.my/12228/ |
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