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- W2014092573 abstract "Teleseismic and GPS data were jointly inverted for the rupture process of the 2011 Tohoku earthquake. The inversion results show that it is a bilateral rupture event with an average rupture velocity less than 2.0 km/s along the fault strike direction. The source rupture process consists of three sub-events, the first occurred near the hypocenter and the rest two ruptured along the up-dip direction and broke the sea bed, causing a maximum slip of about 30 m. The large-scale sea bed breakage may account for the tremendous tsunami disaster which resulted in most of the death and missing in this mega earthquake." @default.
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- W2014092573 date "2012-04-01" @default.
- W2014092573 modified "2023-10-09" @default.
- W2014092573 title "Rupture process of the 2011 Tohoku earthquake from the joint inversion of teleseismic and GPS data" @default.
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- W2014092573 doi "https://doi.org/10.1007/s11589-012-0839-1" @default.
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