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   "name": "High\u2010frequency rupture processes of the 2014 Mw 8.2 Iquique and 2015 Mw 8.3 Illapel, Chile, earthquakes determined from strong\u2010motion recordings",
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       "value": "10.1785/0120210331",
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     "name": "Bulletin of the Seismological Society of America",
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     "issueNumber": "4"
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   "datePublished": "2022",
   "dateModified": "2022-08-29",
   "abstract": "Strong\u2010motion recordings of the 2014\u00a0MwMw\u00a08.2 Iquique and 2015\u00a0MwMw\u00a08.3 Illapel, Chile, earthquakes were analyzed to determine rupture propagation and the location, timing, and strength of subevents that produce most of the high\u2010frequency (\u22651\u00a0Hz) ground motions. A moving window,cross\u2010correlation analysis of recordings from a local dense array, band\u2010pass filtered at 1\u00a0Hz, directly shows that the Iquique earthquake ruptured to the southeast over a distance of about 60\u00a0km. Array analysis of lower frequency energy (0.03\u20130.1\u00a0Hz) indicates that it occurred updip of the high\u2010frequency rupture. A methodology was developed for inverting the envelopes of acceleration records (1\u20135\u00a0Hz) to map high\u2010frequency source factors on the rupture zone and was applied to the two earthquakes. Waveforms of\u00a0MwMw\u00a06 earthquakes were used as empirical Green\u2019s functions in the inversions. High\u2010frequency subevents within the two\u00a0MwMw\u00a08 earthquakes were located at depths ranging from 25 to 55\u00a0km and mostly occurred downdip of the peak slip of these earthquakes. Fourier spectral ratios of the Iquique mainshock with respect to\u00a0MwMw\u00a05\u20136 aftershocks were fit to determine their stress drops. The stress drops were roughly constant from\u00a0MwMw\u00a05 to 8 at 10\u201320\u00a0MPa. A compound rupture model is described in which subevents occur in areas of spatially heterogeneous strength and stress on the rupture, and produce the high\u2010frequency radiated energy of the overall earthquake, but are not located in the areas of peak slip. The stress drop of the overall earthquake is shown to equal the root mean square stress drop of subevents averaged over the rupture area.",
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