Tectonic evolution of the Malay and Penyu Basins, offshore Peninsular Malaysia
<p>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 d...
Main Author: | Madon, M |
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Other Authors: | Dewey, J |
Format: | Thesis |
Language: | English |
Published: |
1995
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Subjects: |
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