supported by the National Key Research and Development Project of China(No.2021YFC3000600)。
The Longmenshan structural belt on the eastern edge of the Tibetan Plateau experienced the impactful Mw7.92008 Wenchuan Earthquake,causing a 350 km surface rupture.Traditional models attribute this to the Beichuan and...
supported by the National Natural Science Foundation of China(Grant Nos.41941016,U1839204,42074105);the National Key R&D Program of China(Grant No.2018YFC1504104);the special project for Basic Scientific Research Business of the National Institute of Natural Hazards,Ministry of Emergency Management(Grant No.ZDJ2019-20)。
In the Longmenshan thrust belt,the Dayi seismic gap,an area with few earthquakes,is located between the ruptures of the 2008 Wenchuan Earthquake and the 2013 Lushan Earthquake,with a length of approximately 40–60 km....
Supported by the National Natural Science Foundation of China(41872143);National Science and Technology Major Project of China(2016ZX05007-004);PetroChina Science and Technology Major Project(2016E-0604)。
By integrating surface geology,seismic data,resistivity sections,and drilling data,the structural deformation characteristics of the frontier fault of thrust nappes were delineated in detail.The frontier fault of thru...
supported by the National Key R & D Program of China (Grant No. 2017YFC1500305);the National Natural Science Foundation of China (Grant Nos. 41731072 & 41574095)
The Longmenshan fault, which defines the eastern edge of the Tibetan Plateau, is one of the steepest margins of the plateau with a sharp elevation drop of about 4 km over a distance less than 100 km across the Longmen...
The 2008 Wenchuan earthquake resulted in a large number of fatalities and caused significant economic losses.Thousands of landslides,many of which are very large,were triggered by the earthquake.A majority of catastro...
the National Key R&D Program of China(No.2016YFC0600301);the National Natural Science Foundation of China.(No.41974053).
The Longmenshan fault zone(LMSF),characterized by complex structures and strong seismicity,is located at the junction between the eastern margin of the Tibetan Plateau and the north-western Sichuan basin.Since the Wen...
jointly supported by the National Natural Science Foundation of China(grant No.41602206);the International Science&Technology Cooperation Program of China(grant No.2011DFG23400)
Objective The occurrence of the devastating Wenchuan earthquake not only caused huge economic loss and deaths but also raised a question whether or not it would trigger any destructive earthquakes on its neighboring s...
supported by a grant from the Chinese Earthquake Administration (No.201308013);the National Natural Science Foundation of China (Nos.41604057, 40974034, and 41021003);a key project from the Institute of Geodesy and Geophysics
On April 20, 2013, an M_s 7.0 earthquake struck Lushan County in Sichuan Province, China, and caused serious damage to the source region. We investigated the rupture process of the M_s7.0 Lushan earthquake by jointly ...
supported by the National Natural Science Foundation of China(grant No.41302159)
Objective The uplift process and uplift mechanism of the Tibetan Plateau has been a research focus among geologists in recent years. This work put emphasis on the Cenozoic exhumation histories of the blocks bounded by...
China Seismic Active Fault Exploration,Central–South Segment Project of North–South Seismic Belt,National Natural Science Foundation of China(grants No.41340005,41372114,41172162,40972083,41502116 and 41402159);the Research Project of Sichuan Education Department(grant No.15ZB0085)for their joint funding
On April 20 th, 2013, an earthquake of magnitude MW 6.6 occurred at Lushan of Sichuan on the southern segment of the Longmenshan fault zone, with no typical coseismic surface rupture. This work plotted an isoseismal m...