Meteoric water leaked and dissolved the lower Paleozoic carbonate rock along faults in Paleogene because of differential upwarding of fault-block.

 
  • 古近紀斷塊發(fā)生差異升降,大氣淡水可以沿斷裂滲流到下古生界碳酸鹽巖中產(chǎn)生溶蝕作用;
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