| 1. | Strike - slip fault
走滑断层 |
| 2. | Visco - elastic model of interaction between parallel strike - slip faults and seismicity reduction effect
平行走滑断层相互作用的粘弹模型和减震作用 |
| 3. | Sinistral strike - slip faults along the southern alashan margin and eastwards extending of the altun fault
阿拉善地块南缘的左旋走滑断裂与阿尔金断裂带的东延 |
| 4. | The radiocarbon ages of charcoal and their implication derived from ciergou site along the haiyuan strike - slip fault
永定河上游晚更新世晚期以来的堆积阶地年代测定 |
| 5. | Recent evidence and of the tangdong tectonic zone strike - slip fault in qikou depressed basin and it ' s significance in exploration
歧口凹陷唐东走滑断裂存在证据及勘探意义 |
| 6. | Mesozoic - cenozoic continental strike - slip fault system and its roles on uranium mineralization in hunan and guangxi , china
湘桂地区中新生代走滑断裂系统对铀成矿的控制作用 |
| 7. | The mesozoic - cenozoic intracontinental strike - slip fault system and the associated hydrothermal uranium mineralization in the border area of eastern hunan and western jiangxi provinces
湘赣边区中新生代走滑断裂系统及对热液铀成矿作用的控制 |
| 8. | The strike - slip faulting was caused by asymmetrical distribution of barriers on the subducting plate . the nne - ssw distributed aftershocks occurred on , or near , the fault plane of the main shock ; while the nw - se distributed aftershocks , on , or near , the mentawai fault
北北东?南南西向分布的余震发生在主震的断层面上(或其附近) ；而西北?东南向分布的余震则发生在明打威断层上(或其附近) 。 |
| 9. | In himalayan , the first era ( 45ma ) the basin is titled ; the second era ( 23ma ) it is differential uplift and denude ; the third era it is brittle defonnation . in eastern ore belt , ore - controlling is mainly strike - slip fault and fold ; but in western ore belt , it is block
喜马拉雅运动第一期45ma盆地掀斜；第二期23ma以差异隆升剥蚀为主；第三期4ma为脆性变形期，东矿带近盆边以走向断裂及褶皱控矿为主，西矿带为断块控矿。 |
| 10. | Considering the ratio of non strike - slip faults and non mainshock - aftershock , yunnan area can be divided into four subareas with different characteristics , which are strike - slip mainshock - aftershock in central yunnan ( a1 ) , incline - slip swarm in northwestern yunnan ( a2 ) , strike - slip double shock in western yunnan ( b1 ) and quasi - strike - slip mainshock - aftershock in southwestern yunnan ( b2 ) , respectively
考虑到非走滑地震断层和非主余震型地震序列所占的比例，可以将云南地区划分为4个具有不同特点的分区：滇中( a1 )走滑主余震型区、滇西北( a2 )斜滑震群型区、滇西( b1 )走滑双震型区和滇西南( b2 )准走滑主余震型区。 |
