Wu-Xia fault belt is a large-scale overthrust belt developed from Late Carboniferous to Triassic and faults mostly develop below the Triassic.

 
  • 烏爾禾-夏子街斷裂帶是一個(gè)晚石炭世至三疊紀發(fā)育起來(lái)的大型逆掩斷裂帶,斷層主要發(fā)育在三疊系以下層位,侏羅系以上近于單斜形態(tài)。
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