2) main hydrocarbon expulsion phase
主排烃期
1.
Thus, the shallow part can accumulate large quantity of hydrocarbon in the main hydrocarbon expulsion phase, which is the key factor for the migration and accumulation of hydrocarbon in the research area.
由此才促使研究区浅部地层在中新世末主排烃期能够聚集大量油气,这也是构成孤岛油田西南缘油气聚集的关键因素。
3) the main stages of hydrocarbon generation and expulsion
主生排烃期
4) hydrocarbon expulsion
排烃
1.
Key factors of controlling the hydrocarbon expulsion of the source rock in Dongying Sag;
控制东营凹陷烃源岩排烃的几个关键因素
2.
Relationships between dynamic conditions of effective hydrocarbon expulsion and critical abundances of organic matter in carbonate source rocks;
碳酸盐岩有效排烃动力条件与临界有机质丰度关系
3.
terogeneity analysis of compaction and hydrocarbon expulsion from source rocks in faulted basin-taking Dongying sag as an example.;
断陷盆地烃源岩压实排烃的非均一性分析——以东营凹陷为例
6) hydrocarbon expulsion threshold
排烃门限
1.
The depth of hydrocarbon expulsion threshold in Fulin subsag is 2250 - 2600m.
富林洼陷排烃门限为2250～2600m,排烃时间从明化镇组沉积末期开始。
2.
Occurrence of hydrocarbon expulsion threshold is discussed by means of geochemical approaches.
排烃门限概念的提出为有效源岩的判识奠定了理论基础 ,它在油气勘探与资源评价中具有重要意义 。
3.
The characteristics of hydrocarbon generation and expulsion of the source rocks in Qaidam basin were experimentally studied by means of the hot pressure physical simulation method and the hydrocarbon expulsion threshold theory.
利用热压物理模拟实验结果并结合排烃门限理论 ,对柴达木盆地各类烃源岩的生、排烃特征进行了模拟实验研究 ,在此基础上绘制了烃源岩排烃门限判别图。
补充资料：大生主
【大生主】
（人名）佛之姨母摩诃波阇婆提Mahaprajapati，旧译曰大爱道，新译曰大生主。玄应音义二十五曰：“大生主，旧言摩诃波阇婆提，翻为大爱道者是也。”
（人名）佛之姨母摩诃波阇婆提Mahaprajapati，旧译曰大爱道，新译曰大生主。玄应音义二十五曰：“大生主，旧言摩诃波阇婆提，翻为大爱道者是也。”
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条