The ARGONET (Greece) Seismic Observatory: An Accelerometric Vertical Array and Its Data
2018; Seismological Society of America; Volume: 89; Issue: 4 Linguagem: Inglês
10.1785/0220180042
ISSN1938-2057
AutoresN. Theodoulidis, Fabrice Hollender, Antonio Joaquín Franco Mariscal, Denis Moiriat, Pierre‐Yves Bard, Agisilaos Konidaris, Edward Marc Cushing, Kiriaki Konstantinidou, Zafeiria Roumelioti,
Tópico(s)earthquake and tectonic studies
ResumoResearch Article| June 06, 2018 The ARGONET (Greece) Seismic Observatory: An Accelerometric Vertical Array and Its Data N. Theodoulidis; N. Theodoulidis aInstitute of Engineering Seismology and Earthquake Engineering (ITSAK‐EPPO), Dassyliou Terma, Eleones, Pylea, GR 55535 Thessaloniki, Greece, ntheo@itsak.gr, kiriaki@itsak.gr Search for other works by this author on: GSW Google Scholar F. Hollender; F. Hollender bFrench Alternative Energies and Atomic Energy Commission (CEA), DEN, CEA Cadarache, DPIE/SA2S, Bât. 352, F‐13108 Saint‐Paul‐lez‐Durance, France, fabrice.hollender@cea.frgAlso at ISTerre, University Grenoble‐Alpes/CNRS/IFSTTAR/IRD/USMB, 38058 GRENOBLE, Cedex 9, France. Search for other works by this author on: GSW Google Scholar A. Mariscal; A. Mariscal cISTerre, University Grenoble‐Alpes/CNRS/IFSTTAR/IRD/USMB, 38058 Grenoble, Cedex 9, France, armand.mariscal@ird.fr, Pierre-Yves.Bard@univ-grenoble-alpes.fr Search for other works by this author on: GSW Google Scholar D. Moiriat; D. Moiriat dIRSN/PSE‐ENV/SCAN, B P 17, 92262 Fontenay‐aux‐Roses, Cedex, France, denis.moiriat@irsn.fr, Edward.CUSHING@irsn.fr Search for other works by this author on: GSW Google Scholar P.‐Y. Bard; P.‐Y. Bard cISTerre, University Grenoble‐Alpes/CNRS/IFSTTAR/IRD/USMB, 38058 Grenoble, Cedex 9, France, armand.mariscal@ird.fr, Pierre-Yves.Bard@univ-grenoble-alpes.fr Search for other works by this author on: GSW Google Scholar A. Konidaris; A. Konidaris eDepartment of Digital Media & Communication, TEI Ionion Nison, A. Tritsi Terma, GR 28100 Argostoli, Greece, konidari@teiion.gr Search for other works by this author on: GSW Google Scholar M. Cushing; M. Cushing dIRSN/PSE‐ENV/SCAN, B P 17, 92262 Fontenay‐aux‐Roses, Cedex, France, denis.moiriat@irsn.fr, Edward.CUSHING@irsn.fr Search for other works by this author on: GSW Google Scholar K. Konstantinidou; K. Konstantinidou aInstitute of Engineering Seismology and Earthquake Engineering (ITSAK‐EPPO), Dassyliou Terma, Eleones, Pylea, GR 55535 Thessaloniki, Greece, ntheo@itsak.gr, kiriaki@itsak.gr Search for other works by this author on: GSW Google Scholar Z. Roumelioti Z. Roumelioti fDepartment of Civil Engineering, Aristotle University of Thessaloniki, University Campus, GR 54124 ?Thessaloniki, Greece, zroum@civil.auth.gr Search for other works by this author on: GSW Google Scholar Author and Article Information N. Theodoulidis aInstitute of Engineering Seismology and Earthquake Engineering (ITSAK‐EPPO), Dassyliou Terma, Eleones, Pylea, GR 55535 Thessaloniki, Greece, ntheo@itsak.gr, kiriaki@itsak.gr F. Hollender bFrench Alternative Energies and Atomic Energy Commission (CEA), DEN, CEA Cadarache, DPIE/SA2S, Bât. 352, F‐13108 Saint‐Paul‐lez‐Durance, France, fabrice.hollender@cea.frgAlso at ISTerre, University Grenoble‐Alpes/CNRS/IFSTTAR/IRD/USMB, 38058 GRENOBLE, Cedex 9, France. A. Mariscal cISTerre, University Grenoble‐Alpes/CNRS/IFSTTAR/IRD/USMB, 38058 Grenoble, Cedex 9, France, armand.mariscal@ird.fr, Pierre-Yves.Bard@univ-grenoble-alpes.fr D. Moiriat dIRSN/PSE‐ENV/SCAN, B P 17, 92262 Fontenay‐aux‐Roses, Cedex, France, denis.moiriat@irsn.fr, Edward.CUSHING@irsn.fr P.‐Y. Bard cISTerre, University Grenoble‐Alpes/CNRS/IFSTTAR/IRD/USMB, 38058 Grenoble, Cedex 9, France, armand.mariscal@ird.fr, Pierre-Yves.Bard@univ-grenoble-alpes.fr A. Konidaris eDepartment of Digital Media & Communication, TEI Ionion Nison, A. Tritsi Terma, GR 28100 Argostoli, Greece, konidari@teiion.gr M. Cushing dIRSN/PSE‐ENV/SCAN, B P 17, 92262 Fontenay‐aux‐Roses, Cedex, France, denis.moiriat@irsn.fr, Edward.CUSHING@irsn.fr K. Konstantinidou aInstitute of Engineering Seismology and Earthquake Engineering (ITSAK‐EPPO), Dassyliou Terma, Eleones, Pylea, GR 55535 Thessaloniki, Greece, ntheo@itsak.gr, kiriaki@itsak.gr Z. Roumelioti fDepartment of Civil Engineering, Aristotle University of Thessaloniki, University Campus, GR 54124 ?Thessaloniki, Greece, zroum@civil.auth.gr Publisher: Seismological Society of America First Online: 06 Jun 2018 Online Issn: 1938-2057 Print Issn: 0895-0695 © Seismological Society of America Seismological Research Letters (2018) 89 (4): 1555–1565. https://doi.org/10.1785/0220180042 Article history First Online: 06 Jun 2018 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation N. Theodoulidis, F. Hollender, A. Mariscal, D. Moiriat, P.‐Y. Bard, A. Konidaris, M. Cushing, K. Konstantinidou, Z. Roumelioti; The ARGONET (Greece) Seismic Observatory: An Accelerometric Vertical Array and Its Data. Seismological Research Letters 2018;; 89 (4): 1555–1565. doi: https://doi.org/10.1785/0220180042 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 ARGOstoli NETwork (ARGONET) consists of a vertical seismic array and a close by (440 m) free‐field station on bedrock, located in Cephalonia, western Greece, in the vicinity of the Cephalonia transform fault zone (CTFZ) that is characterized by a high seismic activity, one of the highest in Europe. It is intended to investigate the effects of local surface geology on the incoming seismic wavefield, with emphasis on strong ground motion (nonlinearity). The vertical array is composed of accelerometer sensors placed on the ground surface at 5.6‐, 15.5‐, 40.1‐, and 83.4‐m depth. The P‐ and S‐wave velocity ranges from surface to bottom bedrock between 600 and 2700 m/s and between 130 and 700 m/s, respectively. The ARGONET started its operation in July 2015. As of 31 December 2017, this array, which operates in continuous mode with Global Positioning System (GPS) absolute time synchronization, has recorded high‐quality recordings for 478 local and regional earthquakes (from ML 1.8 to Mw 6.4 and hypocentral distance from 7 to 180 km, with peak ground acceleration (PGA) from 0.83 to 169 cm/s2). Event dataset along with its metadata are open. The ARGONET data are expected to form the basis for further research on the effects of complex surface geology on ground motion and validation of 1D/2D/3D simulation methods, as well as for studying nonlinear seismic wave propagation phenomena. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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