supported by the Fundamental Research Funds for Central Public Welfare Research Institutes(DF-IGCEA-0608-2-18);the Special Fund for China Earthquake Research Project(201008003)
Relocation result shows that the aftershocks of the Lushan MS7.0 earthquake spatially distribute in a shape like"half bowl",indicating that the rupture structure of the mainshock is a highly curved surface.Kinematic a...
supported by the management and other functions of the Institute of Geology,CEA
As revealed by field investigations,the co-seismic surface rupture zone of the 2010 MS7.1 Yushu earthquake,Qinghai is a characteristic sinistral strike-slip feature consisting of three distinct sinistral primary ruptu...
Supported by the National Key Project of Scientific and Technical Supporting Programs Funded by Ministry of Science & Technology of China (Grant No.2008BAC38B02 and 2006BAC01B02);National Department Public Benefit Research Foundation (Grant No.200708026)
Moment tensor solutions of 88 earthquakes were determined by using the broadband waveform data recorded in six stations within 450 km around the Wenchuan Earthquake sequence by means of the time domain moment tensor i...