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1)  depression type continental basin
拗陷型陆相盆地
2)  depression basin
拗陷盆地
1.
On the basis of that,the sequences filling models of three prototype basins,including early-middle Permian rift basin,late Permian to Triassic piedmont depression,and Jurassic-Cretaceous paracratonic depression basin,were constructed.
结果在研究区划分出2个盆地充填层序,5个一级层序,8个二级层序以及19个三级层序,建立起早中二叠世陆内裂谷盆地、晚二叠世—三叠纪山前拗陷、侏罗纪—白垩纪类克拉通拗陷盆地3个原型盆地的层序充填模式。
3)  continental downfaulted basin
陆相断陷盆地
1.
Discussion on the base level of reservoir-formation in continental downfaulted basin;
陆相断陷盆地成藏基准面探讨
2.
The effect of migration and distribu-tion rule of formation water on well logging inter-pretation in continental downfaulted basin.;
陆相断陷盆地中地层水的运移及分布规律对测井解释的影响
3.
Sequence stratigraphy units at various levels are the results of tectonic movements at various levels and all correspond to petroleum geologic elements with different types at different ways in the continental downfaulted basin.
陆相断陷盆地不同级别的层序地层是不同层次构造运动形式的物质体现,也以不同的方式对应着不同类型的石油地质要素。
4)  continental fault basin
陆相断陷盆地
1.
Distribution and controlling factors of hydrocarbon reservoirs in continental fault basins;
陆相断陷盆地油气藏形成控制因素及分布规律概述
2.
Based on the analysis of fluid pressure and fault characteristicsof continental fault basin,a precise model of abnormal pressure distributionin sagis made.
陆相断陷盆地是中国东部盆地的重要类型,在我国石油勘探开发领域中占有重要地位。
5)  continental faulted basin
陆相断陷盆地
1.
Control of facies-potential coupling on hydrocarbon accumulation in continental faulted basins and its basic geological models;
陆相断陷盆地相-势耦合控藏作用及其基本模式
6)  Continental rift basin
陆相断陷盆地
1.
Seismic characteristics of "five-fan one-channel turbidite" in continental rift basin;
陆相断陷盆地“五扇一沟”的地震响应特征
2.
To pursue the lake-level variation response to tectonic subsidence in the continental rift basin,this paper introduced two parameters(subsidence flux and subsidence velocity flux) to show the whole characteristics of basement subsidence by using two-dimensional stripping-back analysis.
针对陆相断陷盆地构造沉降与湖平面变化的响应关系问题,笔者通过二维回剥分析,并引入沉降通量和沉降速率通量两个参数以评价盆地沉降的整体特征。
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。

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