Mentawai fault zone off Sumatra: A new key to the geodynamics of western Indonesia
M Diament, H Harjono, K Karta, C Deplus… - …, 1992 - pubs.geoscienceworld.org
The geodynamic evolution of the western part of the Sunda arc is controlled by the change
from frontal subduction of the Indo-Australian plate along Java to oblique subduction along
Sumatra. This obliquity gives rise to the Sumatra fault zone that links the accretionary zone
of the Andaman Sea to the Sunda Strait. Previous studies have shown a decrease of
displacement rate of the movement along the fault zone from north to south. Consequently, it
has been proposed that the area between the subduction zone and the fault zone—ie, the …
from frontal subduction of the Indo-Australian plate along Java to oblique subduction along
Sumatra. This obliquity gives rise to the Sumatra fault zone that links the accretionary zone
of the Andaman Sea to the Sunda Strait. Previous studies have shown a decrease of
displacement rate of the movement along the fault zone from north to south. Consequently, it
has been proposed that the area between the subduction zone and the fault zone—ie, the …
[PDF][PDF] Mentawai fault zone off Sumatra: A new key to the geodynamics of western lndonesia
KKLM dan Gas - GEOLOGY, 1992 - researchgate.net
The geodynamic evolution of the western part of the Sunda arc is controlled by the change
from frontal subduction of the Indo-Australian plate along Java to oblique subduction along
Sumatra. This obliquity gives rise to the Sumatra fault zone that links the accretionary zone
of the Andaman Sea to the Sunda Strait. Previous studies have shown a decrease of
displacement rate of the movement along the fault zone from north to south. Consequently, it
has been proposed that the area between the subduction zone and the fault zone-ie, the …
from frontal subduction of the Indo-Australian plate along Java to oblique subduction along
Sumatra. This obliquity gives rise to the Sumatra fault zone that links the accretionary zone
of the Andaman Sea to the Sunda Strait. Previous studies have shown a decrease of
displacement rate of the movement along the fault zone from north to south. Consequently, it
has been proposed that the area between the subduction zone and the fault zone-ie, the …
以上显示的是最相近的搜索结果。 查看全部搜索结果