1) 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。
2) threshold of hydrocarbon expulsion
排烃门限
1.
The threshold of hydrocarbon expulsion is the critical geological condition when hydrocarbon amount generated from the source rock is enough to meet hydrocarbon retention in the source rock itself and begin to be largely expelled.
排烃门限是油气源岩在沉积埋藏过程中生成的油气满足了源岩自身各种形式的残留需要后开始大量排烃的临界地质条件 。
2.
The hydrocarbon expulsion characteristics of two sets of hydrocarbon source rocks --middle-lower Cambrian system (C_(1+2)) source rock and middle-upper Ordovician system (O_(2+3)) source rock in different geologic ages are studied according to the threshold of hydrocarbon expulsion theory and hydrocarbon generation potential.
根据排烃门限理论 ,利用生烃潜力法研究了塔里木盆地台盆区中下寒武统和中上奥陶统 2套烃源岩在不同地质时期的排烃特征 。
3) oil threshold
生烃门限
1.
Combined with the experimental results of previous workers, the present research on the relationships among vitrinite reflectance, burial pressure coefficient, oil threshold, and top gas window indicates that abnormal high pressure not only controls the generative phases of hydrocarbons but also results in reduced maturity of source rock and retarded processes of source rock evolution.
在研究镜质体反射率与地层压力的关系、烃源岩生烃门限深度及石油窗下限深度与地层压力的关系的基础上,结合前人的实验结果研究认为:异常高压不仅影响油气生成的相态,而且降低了烃源岩的成熟度,延缓了烃源岩热演化的进程;当地层压力超过一定的门限时,压力对成烃有明显的抑制作用,表现为压力系数与烃源岩生烃门限深度、石油窗下限深度正相关。
4) thresholds controlling on hydrocarbon
门限控烃
5) the lower limit of hydrocarbon expulsion
排烃下限值
6) 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
补充资料：跳门限
1.指另换门庭。
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