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...
| מחבר ראשי: | |
|---|---|
| מחברים אחרים: | |
| פורמט: | Thesis |
| שפה: | English |
| יצא לאור: |
1995
|
| נושאים: |