1) lithologic trap
岩性圈闭
1.
Analysis of the formation stages of the Paleogene lithologic traps in the southwestern Caidamu Basin;
柴西南区古近系岩性圈闭形成期次分析
2.
Forming conditions and main controlling factors of the Middle-Upper Jurassic lithologic traps on East Fukang Slope,Jungar Basin;
准噶尔盆地阜东斜坡带中上侏罗统岩性圈闭形成条件及成藏主控因素分析
3.
Identification of deep lithologic traps in Middle Junggar Basin;
准中地区深层岩性圈闭识别
2) Lithologic traps
岩性圈闭
1.
Using multi-parameters analysis of seismic information to evaluate lithologic traps in continental basins;
利用地震信息评价陆相盆地岩性圈闭的关键点分析
2.
Application of Jason inversion technique in identification of lithologic traps;
Jason反演技术在岩性圈闭识别中的应用
3.
Prediction of lithologic traps using stochastic simulation;
应用随机模拟方法预测岩性圈闭
3) lithological trap
岩性圈闭
1.
Quantitative prediction of oil - bearing probability in lithological trap of Dongying Sag;
东营凹陷岩性圈闭含油性定量预测
2.
Based on analyzing the genesis types and reservoir-forming course of the lithological trap in the deep sub-depression in downfaulted basin, reservoir-forming mechanism of lithological pool is subtle passage and episodic replacement.
基于断陷盆地深洼区岩性圈闭成因类型分析和成藏过程的研究,指出深洼区岩性油气藏成藏机理主要为隐蔽输导和幕式置换。
3.
Therefore through summing up the volcanic trap models in Xujiaweizi faulted depression(volcanic lithological trap,volcanic facies trap,and volcanic lithological-fault trap),the seismic characteristics of above rock have been understood.
因此,通过总结徐家围子断陷火山岩圈闭模式(火山岩岩性圈闭、火山岩岩相圈闭、火山岩岩性-断层圈闭)认识了火山岩地震响应特征,同时对火山岩储层进行了层位解释及火山岩岩体识别,并应用相干体、地震反演等技术识别出松辽盆地徐家围子断陷营城组火山岩圈闭,从而形成了火山岩圈闭识别方法。
4) stratum-lithology trap
地层-岩性圈闭
1.
Sequence stratigraphy and stratum-lithology trap prediction of the Eh_3 upper member of Hetaoyuan Formation in south Xia'ermen Oilfield,Biyang Sag;
泌阳凹陷下二门地区南部核三上亚段层序地层特征及地层-岩性圈闭预测
5) source-reservoir-caprock assemblage
岩性-构造圈闭
6) lithologic-stratigraphic trap
岩性地层圈闭
1.
Based on the classification of subtle traps in the world, they are divided into three types, namely lithologic-stratigraphic trap, hydrodynamic trap and composite trap.
在参考国内外关于隐蔽圈闭分类的基础上,把隐蔽圈闭分为三类:岩性地层圈闭、水动力圈闭和复合圈闭,岩性地层圈闭又可分为沉积圈闭、成岩圈闭和界面圈闭三种基本类型。
2.
The formation and distribution of lithologic-stratigraphic traps are dependent on the geological structural background, space distribution of strata, special deposition environment of the basin, and the effect of later structure events.
岩性地层圈闭的形成与分布主要取决于盆地的地质构造背景、地层的空间分布、特定的沉积环境及后期构造运动的影响。
补充资料：连续性与非连续性(见间断性与不间断性)
连续性与非连续性(见间断性与不间断性)
continuity and discontinuity
11an父ux泊g四f“山。麻以角g、.连续性与非连续性(c。nt，n琳t:nuity一)_见间断性与不间断性。and diseo红ti-
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