势分布 meaning in Chinese
potential distribution
Examples
- According to those analysis and the background of geological evolution of basin , the kind of hydrodynamics was regarded as compaction before y3 and then as compaction - osmosis after y3 . futhermore , the key time of oil and gas reservoir formation was summarized , it is furthermore , the main cause of high pressure formation was believed that the compaction was not enough in paleogeothermal gradient , meanwhile , analyzing the cause of the low pressure nowadays , it was the uplift and erosion of stratum or pressure divulgence because of seal and so on
另外，还确定油气成藏的关键时期为伊敏组沉积末。再者，认为欠压实是最大埋深状态下，超压形成的主要原因，同时分析了形成现今负(低)压的原因，其原因为地层抬升剥蚀、压力因封闭层的泄漏等。最后，恢复出各主要目的层的古流体势的演化历史，从伊敏组末至现今，油势分布特征具有较好的继承性。 - The main direction and position of petroleum secondary migration is up to potential distribution of fluid . by the simulation computation of the developing profile of palaeofluid potential and the six main conducting path plans of lulehe formation ( period of nowadays , n23 , n22 , n n e3 ) , discovered that eboliang , yahu . lenghumahai structure belts are low potential area in long stage which are petroleum migrating direction area
流体势分布决定了油气二次运移的主要方向和聚集部位，通过模拟计算古流体势发展剖面图和主要输导层路乐河组地层现今、 n _ 2 ~ 3 、 n _ 2 ~ 2 、 n _ 2 ~ 1 、 n _ 1 、 e _ 3等6个时期流体势平面图，发现鄂博梁、鸭湖构造带、冷湖-马海构造带为长期低势区，是油气运移的指向区。