sedimentary compaction

基本解釋

In many sedimentary basins the salinity of the formation water increases with depth or compaction .
在許多沉積盆地中，地層水的含鹽量隨深度或壓實作用而增高。
In combining with the principle of successive sedimentary compaction, a new oil expulsion model known as the compaction-filtration model was established.
提出了烴源巖油水兩相系統(tǒng)相對滲透率計算公式，與逐次沉積壓實排液的原理相結(jié)合，建立了新的排油模型（簡稱壓實滲流模型）。
Voluminous data have demonstrated that there exists close relationship between the degree of compaction of sedimentary rocks and the degree of thermal evolution of organic matter.
大量實際資料證實了沉積巖壓實程度與有機質(zhì)熱演化程度之間存在密切關(guān)系。