Co-seismic fault geometry and slip distribution of the 26 December 2004, giant Sumatra–Andaman earthquake constrained by GPS, coral reef, and remote sensing data
1 Institute of Disaster-Prevention, Sanhe 065201, Hebei, China 2 Department of Earth and Space Sciences, University of California, Los Angeles, CA 90095-1567, USA 3 Institute of Geology, China Earthquake Administration, Beijing 100029, China 4 U. S. Geology Survey, Golden, CO 80401, USA
Co-seismic fault geometry and slip distribution of the 26 December 2004, giant Sumatra–Andaman earthquake constrained by GPS, coral reef, and remote sensing data
1 Institute of Disaster-Prevention, Sanhe 065201, Hebei, China 2 Department of Earth and Space Sciences, University of California, Los Angeles, CA 90095-1567, USA 3 Institute of Geology, China Earthquake Administration, Beijing 100029, China 4 U. S. Geology Survey, Golden, CO 80401, USA
摘要We analyze co-seismic displacement field of the 26 December 2004, giant Sumatra–Andaman earthquake derived from Global Position System observations, geological vertical measurement of coral head, and pivot line observed through remote sensing. Using the co-seismic displacement field and AK135 spherical layered Earth model, we invert co-seismic slip distribution along the seismic fault. We also search the best fault geometry model to fit the observed data. Assuming that the dip angle linearly increases in downward direction, the postfit residual variation of the inversed geometry model with dip angles linearly changing along fault strike are plotted. The geometry model with local minimum misfits is the one with dip angle linearly increasing along strike from 4.3° in top southernmost patch to 4.5° in top northernmost path and dip angle linearly increased. By using the fault shape and geodetic co-seismic data, we estimate the slip distribution on the curved fault. Our result shows that the earthquake ruptured *200-km width down to a depth of about 60 km. 0.5–12.5 m of thrust slip is resolved with the largest slip centered around the central section of the rupture zone 78°N–108°N in latitude. The estimated seismic moment is 8.2 9 1022 N m, which is larger than estimation from the centroid moment magnitude (4.0 9 1022 N m), and smaller than estimation from normal-mode oscillation data modeling (1.0 9 1023 N m).
Abstract:We analyze co-seismic displacement field of the 26 December 2004, giant Sumatra–Andaman earthquake derived from Global Position System observations, geological vertical measurement of coral head, and pivot line observed through remote sensing. Using the co-seismic displacement field and AK135 spherical layered Earth model, we invert co-seismic slip distribution along the seismic fault. We also search the best fault geometry model to fit the observed data. Assuming that the dip angle linearly increases in downward direction, the postfit residual variation of the inversed geometry model with dip angles linearly changing along fault strike are plotted. The geometry model with local minimum misfits is the one with dip angle linearly increasing along strike from 4.3° in top southernmost patch to 4.5° in top northernmost path and dip angle linearly increased. By using the fault shape and geodetic co-seismic data, we estimate the slip distribution on the curved fault. Our result shows that the earthquake ruptured *200-km width down to a depth of about 60 km. 0.5–12.5 m of thrust slip is resolved with the largest slip centered around the central section of the rupture zone 78°N–108°N in latitude. The estimated seismic moment is 8.2 9 1022 N m, which is larger than estimation from the centroid moment magnitude (4.0 9 1022 N m), and smaller than estimation from normal-mode oscillation data modeling (1.0 9 1023 N m).
基金资助:Special Fund of Fundamental Scientific Research Business Expense for Higher School of Central Government (Projects for creation teams ZY20110101), NSFC 41090294 and talent selection and training plan project of Hebei university.
引用本文:
Yongge Wan, Zheng-kang Shen, Min Wang, Yuehua Zeng, Jichao Huang, Xiang Li, Huawei Cui, Xiwei Gao. Co-seismic fault geometry and slip distribution of the 26 December 2004, giant Sumatra–Andaman earthquake constrained by GPS, coral reef, and remote sensing data[J]. 《地震学报》英文版, 2015, 28(3): 187-195.
Yongge Wan, Zheng-kang Shen, Min Wang, Yuehua Zeng, Jichao Huang, Xiang Li, Huawei Cui, Xiwei Gao. Co-seismic fault geometry and slip distribution of the 26 December 2004, giant Sumatra–Andaman earthquake constrained by GPS, coral reef, and remote sensing data. Earthquake Science, 2015, 28(3): 187-195.