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Investigation of offset landforms and trench excavation are important means to acquire the evidence of multistage activi......
Coseismic vertical deformation of the M_S8.0 Wenchuan earthquake from repeated levelings and its con
The devastating MS8.0 Wenchuan earthquake ruptured two large parallel thrust faults along the middle segment of the Long......
The late Pli cene freshwater Taiku Deposits developed in tnebasin behind the great Taiku fault-scarp in central Shansi,......
INTRODUCTION Looking east across the Yüho from the higher ground around Tatungfu, the eye is caught by a dome-shaped h......
Paleoseismology was originated in the late nineteen century, but the modern paleoseismology formed at the end of the 19......
Colluvial wedges collapsed from fault scarp can also be used to study reverse faulting paleoearthquakes. Generating pro......
History of Paleoseismic ActivityAlong the Hohhot Segment of Daqingshan Piedmont Fault in the Late Qu
A detailed study on geomorphic surfaces and a set of trenches on the Hohhot segment of Daqingshan piedmont fault at thre......
Through studying eighteen trenches along the Haiyuan fault, ten paleoearthquakes since ten thousand years ago were deter......
Preliminary study on active features of Fenghuangshan-Tianshui fault, West Qinling north boundary fa
West Qinling north boundary fault zone (WQNBFZ) is a major NWW-striking fault in the east boundary of Tibetan Plateau, w......
The slip rate and strong earthquake recurrence interval on the Qianning-Kangding segment of the Xian
The geometry of the Qianning-Kangding segment of the Xianshuihe fault zone is quite complex, and it is composed of four ......
The Tianshan Mountains are an important active structural belt in the interior of Eurasia. By integrated methods of sur......
Holocene activities of the Taigu fault zone, Shanxi Province, and their relations with the 1303 Hong
The Taigu fault zone is one of the major 12 active boundary faults of the Shanxi fault-depression system, located on the......
Study on Active Faults and Seismogenic Structure for the 1989 Batang M6.2～6.7 Earthquake Swarm in th
Fault structures in the Litang-Batang region of West Sichuan are mainly sub-longitudinal and a set of NNE- and NW-trendi......
Average slip rate, earthquake rupturing segmentation and recurrence behavior on the Litang fault zon
The Litang fault zone (LFZ) is an active fault zone within the northwestern Sichuan sub-block. Field investigation revea......
Based on field investigations and indoor systematic research of the 1879 South Wudu M8.0 earthquake conducted in recent ......
Introduction The Tanlu fault zone lies in the eastern China, which is an important huge active fault with a long history......
The East Kunlun active fault is an important NWW-trending boundary fault on the northeastern margin of the Qinghai-Xizan......
Basic Characteristics of Active Structures in Western Sichuan and Its Vicinity and Strong Earthquake
Western Sichuan and its vicinity are located in the juncture of three big active blocks, namely, the Chuandian (Sichuan ......
Parameters of Coseismic Reverse- and Oblique-Slip Surface Ruptures of the 2008 Wenchuan Earthquake,E
On May 12th,2008,the M_w7.9 Wenchuan earthquake ruptured the Beichuan,Pengguan and Xiaoyudong faults simultaneously alon......
The maximum coseismic vertical surface displacement and surface deformation pattern accompanying the
The amount of coseismic deformation and its distribution of the Wenchuan earthquake provide important scientific bases f......
According to a new investigation in the northern Hexi corridor,the remains of two surface rupture zones were discovered ......
Research on the Historical Data of the 1585 A. D. South Chaoxian Earthquake and Its Seismogenic Stru
In 1585,a MS5 3/4 earthquake occurred in the south of Chaoxian county,Anhui Province. The parameters of this earthquake ......
Late Quaternary Activity and Paleoearthquakes along the Nanyukou Segment of the Northern Piedmont Fa
The northern piedmont fault of Wutai Mountain is located at the north of the Shanxi Graben system,which is the dominatin......
Near-field postseismic deformation along the rupture of 2008 Wenchuan earthquake and its implication
At first time,we observed the postseismic deformation,which actually is a kind of creep after slip,along the intra-plate......
Focusing Seismic Energy along Faults through Time-Variable Rupture Modes: Wenchuan Earthquake, China
Field analysis and differential interferometry derived from Synthetic Aperture Radar (PALSAR) of the epicentral area of ......
On April 14,2010,a devastating earthquake measured 7.1 on the Richter scale struck Yushu county,Qinghai Province,China.F......
Late Pleistocene-Holocene slip history of the Langshan-Seertengshan piedmont fault(Inner Mongolia,no
Offset geomorphic features and deformed late Quaternary strata indicate active deformation along the Langshan-Seertengsh......
The Qian-Gorlos earthquake, which occurred in the Songliao basin in Jilin Province in 1119 AD, was the largest earthquak......
A study has been made of the paragenetic relations of the pediments and river terraces on the northern piedmont of Wutai......
Xizhang trench is located 10 km northwest of Taiyuan city,Shanxi Province,in front of a NNW-trending scarp of 4.6m heigh......
The results from investigation of large quantity of fault outcrops and artificial earthquakes suggest that the Lin-tong-......
Analysis of fault outcrops and trench sections indicates fault displacements of 0.2m～6.0 m on the bottom paleosol layer o......
In the paper, an exploration is made by the techniques of shallow seismic prospecting, borehole composite profile analys......
Using borehole core analysis to reveal Late Quaternary paleoearthquakes along the Nankou-Sunhe Fault
The Nankou-Sunhe Fault is a buried active normal fault that traverses the urban area of Beijing.Its seismic risks have c......
Surface deformation at the epicenter of the May 12,2008 Wenchuan M8 Earthquake,at Yingxiu Town of Si
Surface deformation,along National Highway 213 at the epicenter of Wenchuan M8 earthquake,at Yingxiu Town of Sichuan Pro......
Study of Paleoearthquakes by Excavation of Grouped Trenches on the Zemuhe Fault in Daqingliangzi,Xic
Uncertainties are common in the dating of paleoearthquakes.To improve the credibility of the dating of paleoearthquakes,......
The Characteristics and Cause of Seismic Damage of the Jinghe M5.0 Earthquake in Xinjiang on October
The epicenter of the M5.0 earthquake occurring in Jinghe County, Xinjiang on October 16, 2011, is located in Tuoli Towns......
Although there are many earthquake relics preserved in the southeast segment of the Ganzi-Yushu Fault in the central Tib......
Influences of pre-existing fracture on ground deformation induced by normal faulting in mixed ground
Physical model tests have been conducted by various researchers to investigate fault rupture propagation and ground defo......
The SPOT image analysis in Muzaffarabad Azad Kashmir,northwest Himalayas,Pakistan reveals that the Kashmir earthquake 20......
EVIDENCE OF NEOTECTONIC IMPACT ON A LARGE SEDIMENTARY BASIN BETWEEN TIBETAN PLATEAU AND GOBI ALTAY,N
The Ejina( Gaxun Nur) Basin-enclosed by the Tibetan Plateau in the south and the Gobi Altay in the north hascontinuousl......
Recent Activity of the Badu-Longwei Segment,Guguan-Xiangong Fault in Southern Liupanshan,Constrained
This study’s objective was to investigate the Guguan-Xiangong Fault, which lies in the southern Liupanshan area, throug......
Mass transport deposits and processes in the north slope of the Xisha Trough,northern South China Se
Triple mass-transport deposits(MTDs) with areas of 625, 494 and 902 km2, respectively, have been identified on the north......
Holocene activity evidence on the southeast boundary fault of Heqing basin, middle segment of Heqing
The Heqing-Eryuan fault is an important part of the active fault system in the Northwestern Yunnan Province, China. Thus......
Deformation of the Most Recent Co-seismic Surface Ruptures Along the Garzê–Yushu Fault Zone(Dangjian
The Garzê–Yushu strike-slip fault in central Tibet is the locus of strong earthquakes(M > 7). The deformation and geom......
At 5: 39 AM on 24 June 2017, a huge landslide-debris avalanche occurred on Fugui Mountain at Xinmo village, Diexi town, ......
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7......
Kazkeaerte fault zone is recognized as an important boundary between Pamir and Tianshan Cenozoic Mountain belts in the w......
