1) fault-sagduction basin model
断陷盆地构造模式
2) graben style basin
地堑式断陷盆地
1.
Chaluhe Fault Depression of the Yitong Graben is an graben style basin.
伊通地堑属佳—伊地堑的南段,是郯庐断裂带的北延部分,其内的岔路河断陷为一典型的地堑式断陷盆地。
3) rifted basin
断陷盆地
1.
Episodic tectonic cycles and sequence pattern of the Tertiary rifted basins of East China;
中国东部第三系典型断陷盆地幕式构造旋回及层序地层特征
2.
Multiplex buried-hill genesis and pool-forming in rifted basin;
断陷盆地多样性潜山成因及成藏研究——以济阳坳陷为例
3.
Dynamic hydrocarbon accumulation systems and hydrocarbon distribution in rifted basin: a case of North Jiangsu basin;
断陷盆地成藏动力系统特征与油气分布规律——以苏北盆地为例
4) fault basin
断陷盆地
1.
Analysis on reservoir forming of interlayer geologic body in fault basin:A case study on Beizhong sub-depression in Hailaer Basin;
断陷盆地层间地质体成藏分析——以海拉尔盆地贝中次凹为例
2.
"Facies-potential-transport" reservoir model and formation of reservoirs in fault basin;
断陷盆地“相-势-导”成藏模式与油气成藏
3.
Research on history of gas migration and accumulation in fault basin: Taking Wen 23 Gas Field of Dongpu Depression as an example;
断陷盆地天然气运聚成藏史研究——以东濮凹陷文23气田为例
5) faulted basin
断陷盆地
1.
The Types and the characteristics of the double-fault depressions in the continental faulted basins in east China;
中国东部陆相断陷盆地双断凹陷类型及特征
2.
Sequence stratigraphy analysis and lithologic-stratigraphic reservoir predication in deepwater faulted basins——an example from the Paleogene T Formation of the deepwater C Basin in South China Sea
深水断陷盆地层序地层分析与岩性-地层油气藏预测——以中国南海C盆地深水区古近系T组为例
3.
The heterogeneity of hydrocarbon fluid movement in faulted basin
断陷盆地烃类流体运动的非均一性
6) downfaulted basin
断陷盆地
1.
Dynamics pattern of lithological oil-gas pool forming in subsag belt, downfaulted basin——taking Jiyang Depression as an example;
断陷盆地洼陷带岩性油气藏成藏动力学模式——以济阳坳陷为例
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。
补充资料：断陷盆地
断陷盆地
指断块构造中的沉降地块，又称地堑盆地。它的外形受断层线控制，多呈狭长条状。盆地的边缘由断层崖组成，坡度陡峻，边线一般为断层线。随着时间的推移，在断陷盆地中充填着从山地剥蚀下来的沉积物，其上或者积水形成湖泊（如贝加尔湖、滇池），或者因河流的堆积作用而被河流的冲积物所填充，形成被群山环绕的冲积、湖积、洪积平原。如太行山中的山间盆地和地堑谷中发育着的冲积洪积平原。低于海平面的断陷盆地被称为大陆洼地。
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