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  • 1
    Publikationsdatum: 2015-10-29
    Beschreibung: Central Nepal was struck on 25 April 2015 by the M w  7.8 ( M L  7.6) Gorkha earthquake, which initiated about 80 km northwest of Kathmandu and ruptured toward the east along a 140-km-long west-northwest–east-southeast fault segment. Kathmandu basin, located about halfway along the ruptured segment a few kilometers from the southernmost fault tip, was strongly affected. In this article, we present a preliminary analysis of the acceleration-time histories of the 25 April 2015 M w  7.8 mainshock and the 12 May 2015 M w  7.3 ( M L  6.8) aftershock recorded at the Department of Mines and Geology office building in central Kathmandu valley. We analyze their frequency content using Stockwell et al. (1996) time–frequency decomposition and a polarization analysis ( Pinnegar, 2006 ). We then compute their strong-motion parameters and finally compare their spectral accelerations with the Boore and Atkinson (2008) ground-motion prediction equation.
    Print ISSN: 0895-0695
    Digitale ISSN: 1938-2057
    Thema: Geologie und Paläontologie
    Standort Signatur Erwartet Verfügbarkeit
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  • 2
    Publikationsdatum: 2018
    Beschreibung: 〈span〉〈div〉ABSTRACT〈/div〉The Mw 6.2 Amatrice earthquake that struck central Italy on 24 August 2016 was recorded by seven infrasound arrays in the Euro‐Mediterranean region at distances up to 1260 km. Most stations recorded long‐lasting coherent wavetrains characterized by large back‐azimuth variations. The backprojection of the stratospherically ducted infrasound recorded at five arrays illuminates radiating regions over ∼600  km along the Apennines from the Po basin to the Gulf of Naples. A comparison between the acoustic surface pressure derived from infrasound records and the seismic source pressure derived from measured seismic ground motion shows first‐order agreement in the attenuation with the epicentral distance. From these observations, seismic quality factors in central Italy are estimated. The northernmost reconstructed source region comprises the Po Valley where seismic amplification occurred within the plain alluvial sediments. These results show that infrasound records at hundreds of kilometers from a shallow moderate magnitude devastating earthquake can provide ground shaking information as well as local amplification caused by topographic and geological features.〈/span〉
    Print ISSN: 0895-0695
    Digitale ISSN: 1938-2057
    Thema: Geologie und Paläontologie
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
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