1.
Electron Spin Resonance Dating and Strike-Slip Characteristics of the Daquan Fault in the Beishan Area on the Border between Xingjiang and Gansu Provinces
新甘交界北山地区大泉断裂走滑特征及ESR测年证据
2.
SLIP DISPLACEMENT AND ITS RATE ABOUT ZEMUHE FAULTS
则木河断裂带的走滑位移及滑动速率
3.
rhegmatic pattern
区域性走向滑移断裂模式
4.
second group,strike 195°,dip 80°,rake -165°
第二条断裂,走向195°,倾角80°,滑动角—165°。
5.
3D finite element simulation on sinistral strike-slip of Dunhua-Mishan fault
敦-密断裂左行走滑三维有限元模拟
6.
The application of strike slip fault identification technique in Liaodong exploration area
走滑断裂识别技术在辽东探区的应用
7.
RELATIONSHIP BETWEEN MIDDLE TANLU STRIKE SLIP FAULT BELT AND OIL-AND-GAS ACCUMULATION IN XINTAN AREA
郯庐中段走滑断裂与新滩地区油气成藏关系
8.
Geodynamic mechanism of dextral strike-slip of the western-edge faults of the South China Sea
南海西缘断裂带右行走滑的地球动力学机制
9.
Sudden rupture and displacement occurs with normal, reverse, strike-slip, or oblique-slip faulting.
突然破裂和位移伴随正、逆、走向滑动或斜向滑动断层作用而发生。
10.
QUANTITATIVE EVALUATION OF FRACTURE DISTRIBUTION IN THE DOWN STRIKE-SLIP FAULT ZONE OF UPPER SHUAIBA MEMBER OF LOWER CRETACEOUS,DALEEL,OMAN
阿曼Daleel油田下白垩统Shuaiba组上段走滑正断裂带裂缝分布定量评价
11.
Study on strike-slip structural features of Xiaokuan faulted zone in Shiwu fault depression and analysis on its exploration perspective
十屋断陷小宽断裂带的走滑特征研究及其勘探前景分析
12.
The strike-slip-thrust fault strikes to 280-305°and the fault plane dips to southwest with angle of about 30°.
走滑逆断层走向为280°—305°。
13.
MOSHA BASIN IN WEST YUNNAN: A NEOGENE TRANS-RELEASING BASIN CONTROLLED BY THE RED RIVER FRACTURE
受红河断裂控制的晚第三纪走滑松弛盆地——以漠沙盆地为例
14.
Tectono-Thermochronology Study on Strike-Slip Movement in the Middle-Southern Segment of Tan-Lu Fault Zone;
郯庐断裂带中—南段走滑运动的构造—热年代学研究
15.
Structural Characteristics of the Dien Bien Phu Strike Slip Fault Zone and Its Regional Tectonic Implication
奠边府走滑断裂带的构造特征、遥感解译及其区域构造意义
16.
Characteristics and modeling of the Cenozoic right-lateral slip deformation in the Liaodong Bay segment of the Tan-Lu fault zone
郯庐断裂带辽东湾段新生代右旋走滑变形及其模拟实验
17.
Strike-slip Structural Feature and Its Influence on the Hydrocarbon Accumulation in Kendong Area,Jiyang Depression
济阳坳陷垦东走滑断裂构造特征及其对油气成藏的影响
18.
The northern piedmont fault of the Liulengshan Range lies along the southern edge of Yangyuan basin.
六棱山北麓断裂位于阳原盆地南缘，是一条总体走向北东东、倾向北北西的倾滑正断裂。