Landsliding and the evolution of normal-fault-bounded mountains
نویسندگان
چکیده
منابع مشابه
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چکیده ندارد.
strain analysis of the darvazeh quran fault, zagros mountains, iran
the zagros fold-and-thrust belt is tectonically active and often has active faults with insensible and slow motions. determining the rate of movement and displacement in these faults requires very precise measurements. one of the measurement methods of fault movements is using geodetic and micro-geodetic studies. this research is focused on one of the active faults in the north of shiraz city, ...
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ژورنال
عنوان ژورنال: Journal of Geophysical Research: Solid Earth
سال: 1998
ISSN: 0148-0227
DOI: 10.1029/98jb00510