压实作用 compaction
- 在许多沉积盆地中,地层水的含盐量随深度或压实作用而增高。
In many sedimentary basins the salinity of the formation water increases with depth or compaction. - 压实作用较弱则利于孔隙的保留和产生,能发育良好的储集层,而不利于有机质的转化。
Therefore, the weak compaction is favourable for the development of good reservoirs, but disadvantageous to the transformation of organic matter. - 烃类生成、压实作用,蒙脱石脱水,水热增压及地层的封闭性是产生高压油气藏的主要原因。
The major causes of abnormally high pressure oil-gas pools are hydrocarbon generation, under compaction, montmorillonite dehydration, hydrothermal-pressure increasing and sealing.
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