Item talk:Q244969

From geokb

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   "name": "Rupture history of the 2011 M 9 Tohoku Japan earthquake determined from strong\u2010motion and high\u2010rate GPS recordings: Subevents radiating energy in different frequency bands",
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   "abstract": "Strong\u2010motion records from KiK\u2010net and K\u2010NET, along with 1\u00a0sample/s Global Positioning System (GPS) records from GEONET, were analyzed to determine the location, timing, and slip of subevents of the\u00a0M\u00a09 2011 Tohoku earthquake. Timing of arrivals on stations along the coast shows that the first subevent was located closer to the coast than subevent (2), which produced the largest slip. A waveform inversion of data from 0 to 0.2\u00a0Hz indicates that the first subevent primarily ruptured down\u2010dip and north of the hypocenter and had an\u00a0M\u00a0of 8.5. The areas of this subevent that generated the low (<0.2\u2009\u2009Hz) and high (>0.2\u2009\u2009Hz) frequency energy are located in the same vicinity. The inversion result for the second subevent (M\u00a09.0) has large slip on the shallow part of the fault with peak slip of about 65\u00a0m above about 25\u00a0km depth. This slip generated the tsunami. The preferred inversion has initiation of subevent 2 on the shallow portion of the fault so that rupture proceeded down\u2010dip and mainly to the south. Subevent 2 started about 35\u00a0s after subevent 1, which allows for the possibility of dynamic triggering from subevent 1. The slip model predicts displacements comparable to those found from ocean\u2010bottom transducers near the epicenter. At frequencies that most affect tall buildings (0.1\u20130.5\u00a0Hz), there is a strong pulse (subevent 3) in the strong\u2010motion records that arrives after the near\u2010field ramp from subevent 2. High\u2010frequency subevent 3 was located down\u2010dip and south of the high\u2010slip portion of subevent 2 and was initiated as rupture from subevent 2 proceeded down\u2010dip. The compact pulse for subevent 3 is modeled with an\u00a0M\u00a08.0 source in a 75 by 30\u00a0km area that ruptured down\u2010dip and to the south with a high slip velocity, indicating high stress drop.",
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