Benjamin Sautter, Manuel Pubellier, Pierre Jousselin, Paolo Datt, . (2016) Late Paleogene rifting along the Malay Peninsula thickened crust. Late Paleogene rifting along the Malay Peninsula thickened crust .
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Official URL: http://www.sciencedirect.com/science/article/pii/S...
Abstract
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. Several stages of rifting have been documented thanks to extensive geophysical exploration.
Item Type: | Article |
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Subjects: | Q Science > QE Geology |
Academic Subject One: | Academic Department - Petroleum Geosciences - Petrophysics - Petrophysical data acquisition |
Departments / MOR / COE: | Departments > Geoscience & Petroleum Engineering |
ID Code: | 12228 |
Deposited By: | Mr Ahmad Suhairi |
Deposited On: | 05 Jun 2017 08:05 |
Last Modified: | 05 Jun 2017 08:05 |
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