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Publications (6)
We present the first probabilistic seismic hazard assessment (PSHA) specifically for the Shanxi rift system, north China, which has been defined as one of the areas of highest seismic hazard and risk in China in recent decades. We applied a Monte Carlo-based approach to PSHA, based on so far the most complete earthquake catalog available, a detaile...
Published results of coda Q show a large variation in values. These variations are often claimed to be related to different tectonics, whereas they might just be related to using different assumptions in the processing, leading to different input parameters for the analysis. In this study, the effect of using different processing parameters is inve...
A comprehensive study on regional stress field around the Taigu fault zone in Shanxi Province, China, was performed in this study. To get a better understanding of the present-day stress status in this area, 31 focal mechanisms of M
L ≥3 earthquakes since 1965 were compiled, and the best stress tensor was then inverted based on the database. Additi...
The Shanxi rift system is one of the most active intraplate tectonic zones in the North
China Block, resulting in devastating seismicity. Since 1303, the rift has experienced fifteen
Ms ≥ 6.5 earthquakes. Aiming at a better understanding of Coulomb stress evolution and its
relationship with the seismicity in the rift system, we investigated the Cou...
Earthquake focal mechanisms of the Shanxi rift system, North China, are investigated for the time period 1965-April 2014. A total of 143 focal mechanisms of ML ≥ 3.0 earthquakes were compiled. Among them, 105 solutions are newly determined in this study by combining the P-wave first motions and full waveform inversion, and 38 solutions are from ava...
A new locally calibrated M L scale was derived for the area around the Shanxi rift system, North China, from 83 events recorded on 56 stations of the Shanxi Seismic Network (SSN) resulting in 2,633 observations during the period of 2008–2012. It is expressed as M L = log(A) + 0.80log(R) + 0.00187R − 1.4, where A is the maximum amplitude of vertical...