TY - JOUR
T1 - Relocation of small to moderate earthquakes in Shanxi Province and its relation to the seismogenic structures
AU - Song, Mei Qin
AU - Zheng, Yong
AU - Ge, Can
AU - Li, Bin
PY - 2012/2/20
Y1 - 2012/2/20
N2 - Based on the phase reports of analog seismic stations from 1981-2001, and those of digital seismographs from 2002-2008, we relocated the small to moderate earthquakes with unprecedented precision by absolute and relative relocating methods. Results show that: (1) comparing with precious researches, the percentage of relocated earthquakes with horizontal locating error ≤5 km increases from 65. 8% to 86. 2%, and 7498 earthquakes which were not located previously are located in this work; (2) The general pattern of seismicity has no big changes in horizontal directions. Most earthquakes occurred in the central rift belt, with a few earthquakes located at the two sides of the Fenhe-Weihe Rift While in vertical direction, the relocated earthquakes have an obvious trend that the earthquake depths increase from north to south part of the Fenhe Rift (3) The distribution of relocated earthquakes can outline the profile of the lower seismogenic boundaries of the basins, as well as the boundaries between the extensional basins and the uplifted areas. (4) There is a good correlation between the focal depths and the structures of the basin and range system.
AB - Based on the phase reports of analog seismic stations from 1981-2001, and those of digital seismographs from 2002-2008, we relocated the small to moderate earthquakes with unprecedented precision by absolute and relative relocating methods. Results show that: (1) comparing with precious researches, the percentage of relocated earthquakes with horizontal locating error ≤5 km increases from 65. 8% to 86. 2%, and 7498 earthquakes which were not located previously are located in this work; (2) The general pattern of seismicity has no big changes in horizontal directions. Most earthquakes occurred in the central rift belt, with a few earthquakes located at the two sides of the Fenhe-Weihe Rift While in vertical direction, the relocated earthquakes have an obvious trend that the earthquake depths increase from north to south part of the Fenhe Rift (3) The distribution of relocated earthquakes can outline the profile of the lower seismogenic boundaries of the basins, as well as the boundaries between the extensional basins and the uplifted areas. (4) There is a good correlation between the focal depths and the structures of the basin and range system.
KW - Relocation
KW - Seismogenic structure
KW - Shanxi earthquake belt
UR - http://www.scopus.com/inward/record.url?scp=84859137858&partnerID=8YFLogxK
U2 - 10.6038/j.issn.0001-5733.2012.02.014
DO - 10.6038/j.issn.0001-5733.2012.02.014
M3 - Article
AN - SCOPUS:84859137858
SN - 0001-5733
VL - 55
SP - 513
EP - 525
JO - Chinese Journal of Geophysics
JF - Chinese Journal of Geophysics
IS - 2
ER -