The turbidites are mainly developed in the Qingyang, Heshui, Gucheng and Anzhinongchang areas and are controlled by exterior triggering mechanism, aboundant sediment supply, paleo-slope and so on.

 
  • 浊积岩的形成主要受外界的触发机制、充足的物源供给、古斜坡地形等因素控制。
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