z-logo
open-access-imgOpen Access
Slip rates and seismic moment deficits on major active faults in mainland China
Author(s) -
Wang Hui,
Liu Mian,
Cao Jianling,
Shen Xuhui,
Zhang Guomin
Publication year - 2011
Publication title -
journal of geophysical research: solid earth
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2010jb007821
Subject(s) - seismology , geology , slip (aerodynamics) , seismic moment , seismic hazard , mainland china , seismic gap , thrust fault , active fault , moment magnitude scale , fault (geology) , china , geography , geometry , scaling , physics , thermodynamics , mathematics , archaeology
The Chinese mainland features widespread active faults and intensive seismic activity; both can be described in terms of slip rates on these faults. Previous studies of fault slip rates in mainland China have focused on individual faults or fault segments, and large discrepancies exist among results derived from different methods. Here we derive a self‐consistent estimate of the slip rates on all major faults in mainland China using the recently updated GPS data and an elastic block model. The predicted slip rates are high in western and low in eastern China, ranging from 25.1 ± 2.0 mm/yr in the Himalayan Thrust System to less than 1.0 mm/yr in north China. Using these slip rates, we estimated the rates of moment accumulation on the major fault zones and compared them with the seismic moment released on each fault zone using the Chinese historical earthquake catalog that extends for more than 2000 years in many regions. The results show nine seismic zones with large moment deficits (unreleased moment). Future refinement of GPS measurements and earthquake history will allow better estimates of slip rates on individual faults and better assessment of earthquake hazard on these faults in mainland China.

The content you want is available to Zendy users.

Already have an account? Click here to sign in.
Having issues? You can contact us here