An uncompacted belt can be described as an abnormal pore fluid pressure belt surrounded by "shell".
欠压实带可描述成被“壳”包围的一个异常孔隙流体压力带。
The compaction constant is 1.0 for a completely compacted formation and less than 1.6 for an uncompacted formation.
对于完全压实的地层，压实常数为1.0；未压实的地层，压实常数小于1.6。
In a compacted basin, natural hydraulic fracturing is one of the key factors of the pore fluid expulsion of uncompacted belt.
压实盆地中的自然水力破裂是欠压实带孔隙流体排驱的关键因素之一。
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