The main characteristics of the sequences had lots of low-stand fans sand bodies, regionally distributed oil-shale and deep-lacustrine mudstone, and large progradational d.

 
  • 层序的主要特征是发育数量众多的低位扇砂体、区域分布的油页岩和深湖相泥岩及大型的进积三角洲砂体。
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