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  • 1
    Publication Date: 2014-08-08
    Description: A kinematic finite-source study of the 11 May 2011 M w  5.2 Lorca, Spain, earthquake has been performed using broadband data from the Spanish National Network. The nodal plane ambiguity of the double-couple solution was resolved from finite-source analysis, and a rupture velocity of 1.8 km s –1 and the northeast–southwest-striking northwest-dipping plane was found to best fit the data. This fault plane corresponds to the central sector of the Alhama de Murcia fault (AMF). The resulting slip distribution has a maximum of 19.3 cm and a total seismic moment of 6.25 x 10 16 N·m. A Jackknife test has been performed to estimate the fault plane errors and their consequences in the slip distribution. Also synthetic tests have been performed to evaluate the errors in the finite-source modeling. From this model, a prediction of the strong ground motion near the fault, corrected for soil amplification, is given in terms of peak ground velocity (PGV), which fits with the observed value at the accelerograph in the city of Lorca. We also compared the PGV converted to modified Mercalli intensity at the surface with the intensity distribution, also showing good agreement. Finally we extracted the directivity pulse from the strong ground motion record at Lorca with 0.5 s period in the transverse component to the AMF direction and 33 cm s –1 PGV. To further analyze the directivity effect, we estimate the duration and azimuthal amplitude distribution of the source time functions, finding them to be shorter and of greater amplitude in the direction of rupture and longer and smaller in amplitude in the opposite direction.
    Print ISSN: 0037-1106
    Electronic ISSN: 1943-3573
    Topics: Geosciences , Physics
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  • 2
    Publication Date: 2012-02-01
    Description: We present a new automatic earthquake discrimination procedure to determine in near-real time the tectonic regime and seismotectonic domain of an earthquake, its most likely source type, and the corresponding ground-motion prediction equation (GMPE) class to be used in the U.S. Geological Survey (USGS) Global ShakeMap system. This method makes use of the Flinn–Engdahl regionalization scheme, seismotectonic information (plate boundaries, global geology, seismicity catalogs, and regional and local studies), and the source parameters available from the USGS National Earthquake Information Center in the minutes following an earthquake to give the best estimation of the setting and mechanism of the event. Depending on the tectonic setting, additional criteria based on hypocentral depth, style of faulting, and regional seismicity may be applied. For subduction zones, these criteria include the use of focal mechanism information and detailed interface models to discriminate among outer-rise, upper-plate, interface, and intraslab seismicity. The scheme is validated against a large database of recent historical earthquakes. Though developed to assess GMPE selection in Global ShakeMap operations, we anticipate a variety of uses for this strategy, from real-time processing systems to any analysis involving tectonic classification of sources from seismic catalogs.
    Print ISSN: 0037-1106
    Electronic ISSN: 1943-3573
    Topics: Geosciences , Physics
    Location Call Number Expected Availability
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