graben

as a result , the structural study of the two units can help to find out the processes of formation and evolution of yishu graben.

The present Yinchuan graben is not the separated line of Helanshan Basin and Ordos Basin.

Taking Yishu graben as an example, the application of these methods is presented.

and extensional faulted blocks (half graben and half horst) are the main type of structural style.

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.

The FangZheng fault depression lies in the middle north of the Yi-Shu graben of the Song-Liao basin, It's a negative tectonic units.

The Zhangqiang basin is a Late Mesozoic fault sag basin in Northeastern Asia, and is a half-graben, dustpan shaped basin.

The results of le-telling survey show significant subsidence in the graben area before, during and after the seismic active periods.

Moreover, the fundamental mode of the wedge block movement is graben-horst structure.

Faulting formed fault cliff, fault terrace, seabed fault valley, block mountain and graben basin etc.

And the main profile composite patterns are "Y" font, graben, stepladder.

These stations distributed in three tectonic regions, which is Qinling orogenic belt, Weihe graben and Ordos block respectively.

Yitong graben is a strike-slip and extensional basin in Meso-Cenozoic, the eastern China.

Between graben are relatively high-standing blocks called horsts.

A half-graben is a downdropped block bounded by a normal fault on only one side.

The fourth phase is that the NS graben structure was produced by EW expanding mechanism in late Cenozoic.

Jintang mining area of oil shale lies in the central Maoming Basin which is a half- graben basin.

The half graben mode is a main type of depth fault depression of Songliao basin and it is the target for oil-gas exploration.

The Dalianhe oil shale mine lies in the Yuan area of Heilongjiang Province, which is a half graben faulted basin.

Chaluhe fault depression is a graben inland one, where there are 6 third class sequence strati -graphic units.

Gravitational Fields Characteristic in Southeast Guizhou and Geological Significance of Leigongshan Graben System

Sequence Framework Feature and Evolution of the Ramp Belt of Half-Graben-Basin--Example of Jiyang Depression

Sedimentary and sequence characteristics of Paleogene sublacustrine fan of Tangyuan fault depression in Yishu Graben

Topography and Distribution of Central Graben in the Miyoko Section of Okinawa Trough

Contrast Numerical Test of Graben and Horst Influence on Mining Subsidence

Reservoir Sensibility Research on Shuangyang Formation in Moliqing Basin of Yitong Graben

Coseismic Gravity Landforms and Soil Erosion in the Shanxi Graben System

analysis of sequence stratigraphy of eogene system in yi - shu graben

The Latest Horizontal Movement of Shanxi Graben System

Research on Geothermal Resources of Graben-faulting Basin in Hanpingchuan

Characteristics and maturity of crude oil in Yitong graben

A Study on Petrological Features and Genesis of Chaluhe Fault Depression in Yitong Graben in Jilin

Tectonic Styles and Oil-gas Distribution in Yitong Graben

Development of Ground Fissures and Soil Erosion in the Shanxi Graben System

Geology Analysis of Heavy Oil Reservoir on Xing23 Fault-Block in Yitong Graben