欠压实带可描述成被“壳”包围的一个异常孔隙流体压力带。
An uncompacted belt can be described as an abnormal pore fluid pressure belt surrounded by "shell".
川西前陆盆地上三叠统储层具有正常压实和欠压实两种类型。
The Upper Triassic reservoir in west Sichuan foreland basin has experienced normal compaction and ancompaction.
初步分析各时代流体的封闭时间和主要目的层欠压实异常类型。
The confining time of fluids of each age is primarily analyzed as well as sub - compaction anomaly type of the main target layers.
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