It is a collision suture between the Yangtze Block and North China Block during the Indosinian period, a thrust-napping fault zone belonging to the Tethyan regimes in broad sense.

 
  • 在印支期由于揚子地塊與華北地塊的碰撞,成為兩板塊的對接邊界,具有逆沖推覆的性質(zhì),屬廣義的特提斯構造域。
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