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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Bibliografski detalji
Glavni autor: Madon, M
Daljnji autori: Dewey, J
Format: Disertacija
Jezik:English
Izdano: 1995
Teme: