Geodetic slip model of the 2011 M9.0 Tohoku earthquake
The three-dimensional crustal displacement field as sampled by GPS is used to determine the coseismic slip of the 2011 M9.0 Tohoku Earthquake. We employ a spherically layered Earth structure and use a combination of onland GPS, out to ∼4000 km from the rupture, and offshore GPS, which samples the hi...
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Main Authors: | , , |
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格式: | Article |
語言: | English |
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2012
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在線閱讀: | https://hdl.handle.net/10356/94801 http://hdl.handle.net/10220/8799 |
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