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Journal Article

Relationship between High-frequency Radiation and Asperity Ruptures, Revealed by Hybrid Back-projection with a Non-planar Fault Model

Authors

Okuwaki,  R.
External Organizations;
GEOFON, Deutsches GeoForschungsZentrum;

Yag,  Y.
External Organizations;
GEOFON, Deutsches GeoForschungsZentrum;

Hirano,  S.
External Organizations;
GEOFON, Deutsches GeoForschungsZentrum;

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Citation

Okuwaki, R., Yag, Y., Hirano, S. (2014): Relationship between High-frequency Radiation and Asperity Ruptures, Revealed by Hybrid Back-projection with a Non-planar Fault Model. - Scientific Reports, 4, 7120.
https://doi.org/10.1038/srep07120


Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_3222895
Abstract
High-frequency seismic waves are generated by abrupt changes of rupture velocity and slip-rate during an earthquake. Therefore, analysis of high-frequency waves is crucial to understanding the dynamic rupture process. Here, we developed a hybrid back-projection method that considers variations in focal mechanisms by introducing a non-planar fault model that reflects the subducting slab geometry. We applied it to teleseismic P-waveforms of the Mw 8.8 2010 Chile earthquake to estimate the spatiotemporal distribution of high-frequency (0.5–2.0 Hz) radiation. By comparing the result with the coseismic slip distribution obtained by waveform inversion, we found that strong high-frequency radiation can precede and may trigger a large asperity rupture. Moreover, in between the large slip events, high-frequency radiation of intermediate strength was concentrated along the rupture front. This distribution suggests that by bridging the two large slips, this intermediate-strength high-frequency radiation might play a key role in the interaction of the large slip events.