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زمینشناسی و معدن::
فشارشی
crust and /or a zone of compressional structures.
compressional structures with overthrusts evolve
Cosequently, the backarc area is also under compressional stress.
thrust faults that evolved during the compressional phases can be reactivated as normal faults.
Intermedi- ate earthquakes are mostly tensional whereas deep earthquakes are compressional, relative to the direction of the plate movement (Fig. 7.21a,b).
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