Tests of the 2011 Tohoku earthquake source models using free-oscillation data from GOPE |
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Authors: | Eli?ka Zábranová Ctirad Matyska Ladislav Hanyk |
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Institution: | 1. Department of Geophysics, Faculty of Mathematics and Physics, Charles University in Prague, V Hole?ovi?k??ch 2, 180 00, Praha 8, Czech Republic 2. Research Institute of Geodesy, Topography and Cartography, Zdiby, Czech Republic
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Abstract: | Data from a superconducting gravimeter were obtained from the Geodetic Observatory Pecny (GOPE), Czech Republic, and compared with acceleration data from a broadband seismometer at the same location. We calculated synthetic seismograms for several point- and finite-source fast solutions of the 2011 Tohoku earthquake obtained from surface waves and tested them only against the observed gravity data because of high-noise levels in the low-frequency seismic data. We have obtained a good fit of the synthetic amplitude spectrum with the data up to 1.7 mHz without an additional increase of the moment magnitude Mw. In this aspect, the 2011 Tohoku earthquake was similar to the 2010 Maule earthquake and different from the 2004 Sumatra-Andaman earthquake, where the free-oscillations studies resulted in an increase of the early Mw values. The degree-one mode 3S{ia1} dominates the 3S1?C2S2?C1S3 triplet at the GOPE station. |
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