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زمینشناسی و معدن::
آب زدایی
Mud-volcanoes develop by explosive dewatering of sediments under high pressure.
Serpentine dewatering causes intermedi- ate earthquakes to depths of 400 km.
Intermediate earthquakes are related to dewatering processes with increasing depth of the mineral serpentine.
The spontaneous dewatering, which is accompa- nied by a substantial decrease of volume, causes microfracturing and weakens the rock, eventually leading to the formation of shear fractures; they can occur, despite the high lithostatic pressure, if the rock is under directed stress.
belt is considered to be related to the dewatering
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