The Hoh Xil Basin was once an enclosed carbonate-dominated salt lake basin in the xerothermic conditions during the Miocene.

 
  • 總體上為較好的烴源巖,中新世時(shí)可可西里盆地為封閉、干熱的以碳酸鹽巖沉積為主的鹽湖盆地。
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