graben faulting

基本解釋

The development and evolution of the basin was controlled by graben faulting mainly in vertical movement of E-W direction.
以東西向垂直運(yùn)動為主體的構(gòu)造活動控制了盆地的發(fā)展和演化。
The intermountain graben basin that had been formed by the faulting movement was also considered as an active place of seismicity.
山區(qū)因斷裂活動產(chǎn)生的山間斷陷盆地也是地震活動場所。
The evolution of a half graben basin bounded by normal faulting in the upper crust with a Byerlee-type strength envelope has been modelled by elastoplastic finite element analysis.
利用新近完成的粘彈塑構(gòu)造模擬軟件包對盆地的動力學(xué)演化進(jìn)行了一系列模擬。
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