It is recognized that there are calcareous turbidite and autochthonous plankton ammononites bedding in the Ganxi Formation, which provides view evidence on palseontology and sedimentary basin.

 
  • 發(fā)現甘溪組內存在深水相鈣質(zhì)濁積巖及原地埋藏菊石層,為研究古生物、古環(huán)境及沉積盆地演化提供了新資料。
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