The Shulan basin is located in the middle sector of Yilan-Yitong rift, and is a semi-graben basin.
舒兰盆地位于依兰—伊通裂谷中段，为半地堑盆地，依兰—伊通裂谷为盆地的边缘断裂，控制了盆内白垩系及新近系含煤地层沉积。
A series of half graben like faulted basins were developed in Jurassic in the northern edge of Qaidam basin, which was mainly controlled by extensional tectonic framework.
柴达木盆地北缘地区在侏罗纪主要受伸展构造体制控制，发育一系列规模较小的箕状断陷盆地。
The Yitong Graben is a Tertiary petroliferous strike-slip fault basin developed on the Hercynian fold basement.
伊通地堑是一个主体在海西期褶皱基底上发育起来的第三纪含油气走滑断陷盆地。
The Xinding basin in the north of Shanxi rift system is a normal fault-controlled extensional graben and has a strong neotectonic process during the Quaternary.
忻定盆地是山西地堑系北部的一个张性断陷盆地，第四纪构造运动活跃。
The Fuxin basin is a late Mesozoic NNE-trending graben coal-bearing basin.
阜新盆地属于晚中生代nne向地堑式煤盆地。
The Datong Basin is an unsymmetrical graben, the main controlling fault of which runs north east.
大同盆地是一受北东向主干断裂控制的不对称地堑盆地。
Biyang depression is a secondary structural unit in Nanxiang Basin. The depression is in half-graben shape which faulted in the south part and overlapped in the north part.
泌阳凹陷是南襄盆地中的一个次级构造单元，为一南断北超式箕状凹陷。
Uplift in the southwestern Qaidam Basin led to the migration of Middle Jurassic strata to the north and west, and resulted in the formation of inverted haft-graben fault basin.
柴西南隆升导致中侏罗世地层向北、北东迁移，并出现反向箕状断陷盆地。
The present Yinchuan graben is not the separated line of Helanshan Basin and Ordos Basin.
现今的银川地堑当时也并不是贺兰山盆地与鄂尔多斯盆地的分割。
This paper proves the practicality and advantages of the half-graben theory which is a new thinking and a new method in basin analyses.
此文证明了半地堑理论的实用性与优越性，是盆地分析工作中的一种新思路、新方法。
In the Songliao basin there occurred pre-rift volcanic rocks. Then brittle extension of the upper crust gave rise to a semi-graben rift basin.
松辽盆地存在裂谷期前火山岩，之后上地壳脆性伸展发育半地堑裂谷盆地。
In a half-graben, the early-stage movement of the basin-controlling fault results in a great height difference along the lake margin.
在陆相断陷湖盆陡坡带，控盆断裂的剧烈活动导致在相对较短时期内形成盆地的快速沉降，与湖盆边缘地形形成巨大高差。
The structural style found in the basin includes imbricated thrust zone, trapdoor structure, drag fold, listric fault, rollover anticline, horst-graben structure and the like.
盆地中发育多种构造样式，主要有：叠瓦状冲断层、滚板构造、牵引褶皱、铲形正断层、滚动背斜、“垒一堑”构造等。
The structural style found in the basin includes imbricated thrust zone, trapdoor structure, drag fold, listric fault, rollover anticline, horst-graben structure and the like.
盆地中发育多种构造样式，主要有：叠瓦状冲断层、滚板构造、牵引褶皱、铲形正断层、滚动背斜、“垒一堑”构造等。
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