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Late Paleogene rifting along the Malay Peninsula thickened crust

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
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: Ahmad Suhairi
Deposited On:05 Jun 2017 08:05
Last Modified:05 Jun 2017 08:05

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