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...
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| Định dạng: | Luận văn |
| Ngôn ngữ: | English |
| Được phát hành: |
1995
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