The seismic amplitude percentages lower than valve values indicate the range of the deep lacustrine facies.
低于阀值的地震振幅百分比指示了这些深-半深湖相的平面展布范围。
The mudstone reservoir was formed in lacustrine facies of lamellar marl in the deep water or semi-deep water sediment with tensional state.
泥质岩储集层形成于呈拉伸状态的深湖半深湖相纹层状泥灰岩之中。
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