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Published byStella Francis Modified over 5 years ago
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3D path calibration for the 12/30/2009 Imperial Valley Earthquake
Shengji Wei(1), Rob Graves(2), Xiangyan Tian(2), Zhongwen Zhan(2), Eric Fielding(3) and Don Helmberger(1) 1, SeismoLab, GPS, Caltech, Pasadena 2, USGS, Pasadena 3, JPL, Caltech, Pasadena
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Outline 1, Event mechanism from teleseismic and regional inversion
2, Static location and slip model 3, Comparison between 1D, 3D synthetic and the data at different frequency bands for the CVM4m and HVM6.2 models.
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Source mechanism from teleseismic inversion
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Source mechanism from regional seismic inversion
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Static location and Inversion
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1D and 2D profiles from 3D models
Az:310 degree
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Az:310~330, Frequency: 10~100s, Tangential
CVM4m Data 1D HVM6.2
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Az:270~310, Frequency: 10~100s, Tangential
CVM4m Data 1D HVM6.2
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20~200s 1D vs Data 3D(HVM6.2) vs Data 3D(CVM4m) vs Data
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10~100s 1D vs Data 3D(HVM6.2) vs Data 3D(CVM4m) vs Data
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5~100s 1D vs Data 3D(HVM6.2) vs Data 3D(CVM4m) vs Data
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10~100s(vel) 1D vs Data 3D(HVM6.2) vs Data 3D(CVM4m) vs Data
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5~100s(vel) 1D vs Data 3D(HVM6.2) vs Data 3D(CVM4m) vs Data
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