Structural geology of a classic thrust belt earthquake: the 1999 Chi-Chi earthquake Taiwan (Mw=7.6)
Jian-Sheng Yin
Abstract
The 1999 Chi-Chi earthquake is one of the best-instrumented thrust-belt earthquakes. The main surface break and large slip (3¡V10 m) is on two segments of the shallow otherwise aseismic bedding parallel Chelungpu¡VSanyi thrust system, which shows nearly classic ramp-flat geometry with shallow detachments (1¡V6 km) in the Pliocene Chinshui Shale and Mio-Pliocene Kueichulin/Tungkeng Formations. These structural models have been developed using standard structural geologic techniques based on surface geology, seismic lines, well data and balancing concepts and are largely independent of geodeticand seismologic data from the Chi-Chi earthquake and its aftershock sequence. These structural models provide a framework that allows us to assimilate the geodetic and seismologic data into a more realistic image of this classic thrust-belt earthquake than is provided by normal earthquake studies alone. In particular, we have shown that details of the coseismic displacement fields determined from geodesy and seismology correlate significantly with fine details of the 3D fault map of the Chelungpu thrust and that to first order the displacement vectors are parallel to the fault.
Reference
Li-Fan Yue, John Suppe, Jih-Hao Hung, 2005. Structural geology of a classic thrust belt earthquake: the 1999 Chi-Chi earthquake Taiwan (Mw=7.6). Journal of Structural Geology Volume: 27, Issue: 11, November, 2005, pp.2058-2083.
(Abstract)(Full text)
Kaj M. Johnson, Paul Segall, 2004. Imaging the ramp¡Vde¡¦collement geometry of the Chelungpu fault using coseismic GPS displacements from the 1999 Chi-Chi, Taiwan earthquake. Tectonophysics. 378, 123¡V 139.
(Abstract)(Full text)