It is mainly distributed in the fourth part of the Beisi Formation of the lower Triassic, exhibiting tidal flat characteristics and located between the underlying HST and the upper TST.

 
  • 主要見(jiàn)于下三疊統北泗組第四段,具潮坪特點(diǎn),層序上處于下伏的HST和上覆的TST之間。
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