During Devonian Period, the old sea basin of Qinling range was a continental sea, which was situated between Northern China and Yangtz old land.

 
  • 泥盆紀時(shí),奏嶺古海盆是介于華北古陸和揚子古陸之間的一個(gè)復雜的陸表海,故應作獨立地層區。
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