The main fault slop-break zone supplied relatively large accommodation space for the deposition compared with the fault bench slop-break zone, which resulted in relatively great thickness of the sediments and richness in sandstone.

  • 与断阶坡折带相比,主断裂坡折带为沉积作用提供了相对较大的可容纳空间,从而导致主断裂坡折带处的沉积作用以厚度大和砂岩体积分数高为特征。

  • 互联网摘选 2025-01-20 12:54:47

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