Tectonic evolution of the Malay and Penyu Basins, offshore Peninsular Malaysia

Tectonic evolution of the Malay and Penyu Basins, offshore Peninsular Malaysia

The Malay and Penya Basins, offshore Peninsular Malaysia, were formed during the early Oligocene as a result of regional dextral shear deformation caused by the indentation of India into Eurasia in the early Tertiary. Pre-existing basement inhomogeneities exerted a strong control on basin developmen...

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Bibliographic Details
Main Author: Madon, Mazlan B. Hj
Other Authors: Dewey, John F.
Published: University of Oxford 1995
Subjects:
551.21
Earth sciences : Earthquakes and tectonics : Asia : Malay Basin : Penya Basin : geology : thermal history : tectonic subsidence : gravity anomaly : backstripping
Online Access:http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.297278

Internet

http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.297278

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