Besides,study of the sedimentary structure and muddy turbidite shows that Beipeng turbidite basin(T 2 1)was beneath the carbonate compensation depth(CCD),while the Hekou(T 2 2)and Falang(T 1 3)turbidite basins were aere CCD.

 
  • 經(jīng)研究,百蓬期(T21)濁積盆地位于CCD面之下,而河口期(T22)和法郎期(T13)燭積盆地位于CCD面之上。
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