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• W2891997638 abstract "Research Article| September 05, 2018 Estimating the Ground‐Motion Distribution of the 2016 Mw 6.2 Amatrice, Italy, Earthquake Using Remote Infrasound Observations Bruno Hernandez; Bruno Hernandez aCEA, DAM, DIF, F‐91297 Arpajon, France Search for other works by this author on: GSW Google Scholar Alexis Le Pichon; Alexis Le Pichon aCEA, DAM, DIF, F‐91297 Arpajon, France Search for other works by this author on: GSW Google Scholar Julien Vergoz; Julien Vergoz aCEA, DAM, DIF, F‐91297 Arpajon, France Search for other works by this author on: GSW Google Scholar Pascal Herry; Pascal Herry aCEA, DAM, DIF, F‐91297 Arpajon, France Search for other works by this author on: GSW Google Scholar Lars Ceranna; Lars Ceranna bBGR, Stilleweg 2, D‐30655 Hannover, Germany Search for other works by this author on: GSW Google Scholar Christoph Pilger; Christoph Pilger bBGR, Stilleweg 2, D‐30655 Hannover, Germany Search for other works by this author on: GSW Google Scholar Emanuele Marchetti; Emanuele Marchetti cDepartment of Earth Sciences, University of Firenze, Via G. La Pira, 4, 50121 Florence, Italy Search for other works by this author on: GSW Google Scholar Maurizio Ripepe; Maurizio Ripepe cDepartment of Earth Sciences, University of Firenze, Via G. La Pira, 4, 50121 Florence, Italy Search for other works by this author on: GSW Google Scholar Rémy Bossu Rémy Bossu aCEA, DAM, DIF, F‐91297 Arpajon, FrancedAlso at Euro‐Mediterranean Seismological Centre, c/o CEA, DAM, DIF, F‐91297 Arpajon, France. Search for other works by this author on: GSW Google Scholar Author and Article Information Bruno Hernandez aCEA, DAM, DIF, F‐91297 Arpajon, France Alexis Le Pichon aCEA, DAM, DIF, F‐91297 Arpajon, France Julien Vergoz aCEA, DAM, DIF, F‐91297 Arpajon, France Pascal Herry aCEA, DAM, DIF, F‐91297 Arpajon, France Lars Ceranna bBGR, Stilleweg 2, D‐30655 Hannover, Germany Christoph Pilger bBGR, Stilleweg 2, D‐30655 Hannover, Germany Emanuele Marchetti cDepartment of Earth Sciences, University of Firenze, Via G. La Pira, 4, 50121 Florence, Italy Maurizio Ripepe cDepartment of Earth Sciences, University of Firenze, Via G. La Pira, 4, 50121 Florence, Italy Rémy Bossu aCEA, DAM, DIF, F‐91297 Arpajon, FrancedAlso at Euro‐Mediterranean Seismological Centre, c/o CEA, DAM, DIF, F‐91297 Arpajon, France. Publisher: Seismological Society of America First Online: 05 Sep 2018 Online Issn: 1938-2057 Print Issn: 0895-0695 © Seismological Society of America Seismological Research Letters (2018) 89 (6): 2227–2236. https://doi.org/10.1785/0220180103 Article history First Online: 05 Sep 2018 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Bruno Hernandez, Alexis Le Pichon, Julien Vergoz, Pascal Herry, Lars Ceranna, Christoph Pilger, Emanuele Marchetti, Maurizio Ripepe, Rémy Bossu; Estimating the Ground‐Motion Distribution of the 2016 Mw 6.2 Amatrice, Italy, Earthquake Using Remote Infrasound Observations. Seismological Research Letters 2018;; 89 (6): 2227–2236. doi: https://doi.org/10.1785/0220180103 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietySeismological Research Letters Search Advanced Search ABSTRACT 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. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2891997638 date "2018-09-05" @default.
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• W2891997638 title "Estimating the Ground‐Motion Distribution of the 2016 Mw 6.2 Amatrice, Italy, Earthquake Using Remote Infrasound Observations" @default.
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