The differential uplift and subsidence of the crust in the area along the faults resulted in the coexistence of graben valleys,fault block mountains and downfaulted basins.

 
  • 由于本區地殼沿斷裂作差異性升降運動(dòng),造成地塹谷、斷塊山和斷陷盆地并存的地貌特點(diǎn)。
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