1.
Paleoseismic Activity on the Hohhot Segment of Daqingshan Piedmont Fault in the Late Quaternary History
大青山山前断裂呼和浩特段晚第四纪古地震活动历史
2.
Microscopic Marks of Stick Slip and Creep Slippage in Deformation Products along the Daqingshan Piedmont Active Fault
大青山山前活动断裂变形产物中的微观粘滑与蠕滑标志
3.
Survey and Research of Ultra-Long Period Magnetotelluric Sounding in Longmen Mountain Fault Zone
龙门山前山断裂带超长周期大地电磁测深观测研究
4.
CURIE ISOTHERMAL SURFACE AND HEAT FLOW ANALYSIS OF THE ADJACENT REGION OF THE NIANQING TANGGULA PIEDMONT FAULTED ZONES
念青唐古拉山前断裂系周围地区的居里等温面与热流分析
5.
volcanic rift zone
【地质】火山断裂带
6.
Seismological Features of the Segmentation of Nankou Piedmont Fault in Changping County
昌平南口山前断裂断层分段的地震学特征
7.
Lantau Link [formerly known as Lantau Fixed Crossing]
青屿干线〔前称青衣至大屿山干线〕
8.
Magnetotelluric Monitoring of Earthquakes in the Laohushan Fault Zone,Gansu Province
老虎山断裂带大地电磁地震监测研究
9.
Research on the Relationship between the Soil Radon Density and Fault and Geotherm at the Foreland of Jixian Mountain,Tianjing
蓟县山前土壤氡浓度与断裂和地热关系研究
10.
Vertical Deformation Characteristic of Longmenshan Fault Zone before Wenchuan M_S8.0 Earthquake
汶川8.0级地震前龙门山断裂带的垂直变化特征
11.
THE COMPOSITION OF THE WEST SECTION OF THE PIEDMONT FAULT IN NORTH MARGIN OF BOGDA, XINJIANG, MOUNTAINS AND ITS ACTIVITY IN HOLOCENE
新疆博格达山北麓山前断裂西段的断裂组成及其在全新世时期的活动
12.
Average Slip Rate of Daliang Mountain Fault Zone in Sichuan in Late Quaternary Period
四川大凉山断裂带的晚第四纪平均滑动速率
13.
STUDY AND EXPLORATION ON THE DASHITOU SONGSANTAI FAULT IN ANSHAN CITY,LIAONING PROVINCE
辽宁鞍山市大石头宋三台断裂的探测与研究
14.
The Study about Characteristics and Activity of the Faults in Dagang-Mauntain Shimian County;
石棉县大岗山地区断裂特征及活动性研究
15.
Carbon and oxygen isotope features of carbonatite in the main fracture of Daba Mountains foreland structural belt and its fluid response
大巴山前陆构造带主断裂碳酸盐岩碳、氧同位素特征及其对流体的响应
16.
Analysis on Fault Deformation Anomaly of Longmenshan Fault Zone before Ms8.0 Wenchuan Strong Earthquake
汶川Ms8.0级强震震前龙门山断裂带断层形变异常分析
17.
locate in fault basin or sediment basin among plateaus,have deep and great rupture developing and controlling;
均处断陷盆地或高原山间沉积盆地,有深大断裂发育控制;
18.
3、Tectonic style of the orogenic-belt uplift is very complicated,and is markedby the growing of a large number of thrusting rupture and faulted block.
3、造山隆起带构造样式较复杂,发育大量的逆冲断裂与断块体;