Structural evolution of Malay Basin, its link to sunda block tectonics
The Malay Basin is located offshore West Malaysia in the South China Sea, within north central region of 1st order Sunda Block. The basin developed partly as a result of tectonic collisions and strike-slip shear of the Southeast Asia continental slabs, as the Indian Plate collided into Eurasia, and...
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| Main Authors: | , , , |
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| Format: | Article |
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Elsevier Ltd
2014
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| Online Access: | https://www.scopus.com/inward/record.uri?eid=2-s2.0-84918533347&doi=10.1016%2fj.marpetgeo.2014.05.003&partnerID=40&md5=8655ea04e8793bb94f1193f433d3b2f7 http://eprints.utp.edu.my/31070/ |
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