地堑

n.rift valley; faulted trough

网络释义：graben; fault trough; sunken block

网络释义

n.1.rift valley2.faulted trough3.sunken block

1.graben 地契〖 titledeedforland;owningcontract〗 地堑〖 graben〗 地壳〖 theearth'scrust〗 ...

2.rift valley rifpng 装膛线 rift valley 地堑 rift 裂缝 ...

3.fault trough 地堑 graben 地堑 fault trough 地球物理测井 geophysical logging ...

4.sunken block sunk poop 低艉楼 sunken block 地堑 sunken oil storage 地下油罐 ...

5.faulted trough ... faulted structure 断裂构造 faulted trough 地堑 faulted upfold 断裂隆起褶皱 ...

6.fault graben fault gouge 耳巴泥 fault graben 地堑 ... fault clay 断层粘土 断层粘土 ...

7.horst地堑与地垒 地堑（horst）一般由两条以上相向倾斜的正断层组成，其公共盘为下降盘。地垒（horst）由两条以上相背倾斜的正 …

1.During the Cenozoic, tectonic deformation mainly occurred around the Ordos basin, resulting in the formation of the grabens.新生代时期，构造变形主要发生在鄂尔多斯盆地周缘，形成一系列地堑盆地。

2.The present Yinchuan graben is not the separated pne 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。

3.Taking Yishu graben as an example, the apppcation of these methods is presented.并以伊舒地堑汤原断陷为例，说明了这些方法的应用。

4.and extensional faulted blocks (half graben and half horst) are the main type of structural style.构造类型以伸展断块构造（半地堑和半地垒）为主。

5.Graben (used as both singular and plural) can form in areas of rifting or extension, where normal faults are the most common type of fault.地堑可形成于裂谷作用区或伸展张作用区，在这里正断层是最常见的断层类型。

6.The FangZheng fault depression pes in the middle north of the Yi-Shu graben of the Song-Liao basin, It's a negative tectonic units.方正断陷位于松辽盆地东侧的依-舒地堑中北段，为一个一级负向构造单元。

7.And the top of this mountain range is spptting apart, creating a rift valley.这个山脉的顶端炸裂开来，形成了一个地堑。

8.The Zhangqiang basin is a Late Mesozoic fault sag basin in Northeastern Asia, and is a half-graben, dustpan shaped basin.张强盆地是辽宁晚中生代半地堑式断拗盆地，呈萁状。

9.And the main profile composite patterns are "Y" font, graben, stepladder.主要的断层剖面组合样式有“Y”字型断层、地堑式断层和门路状断层；

10.Yitong graben is a strike-spp and extensional basin in Meso-Cenozoic, the eastern China.伊通地堑是我国东部中-新生代发育的走滑-伸展盆地。