Loading…
Near‐source ground motion in the M7.8 Gaziantep (Turkey) earthquake
On the night of February 6, 2023, a major earthquake struck Turkey and nearby Syria, whose moment magnitude (M) was estimated at 7.8 (or 7.7, depending on the data source). It started what can be considered a seismic sequence with thousands of recorded earthquakes with magnitude larger than two, inc...
Saved in:
Published in: | Earthquake engineering & structural dynamics 2023-10, Vol.52 (12), p.3903-3912 |
---|---|
Main Authors: | , , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
cited_by | cdi_FETCH-LOGICAL-c3279-c8aff7a9cfbfebaba8b93c0f61c0770ac594859a51c43f091514ac4725ccd1253 |
---|---|
cites | cdi_FETCH-LOGICAL-c3279-c8aff7a9cfbfebaba8b93c0f61c0770ac594859a51c43f091514ac4725ccd1253 |
container_end_page | 3912 |
container_issue | 12 |
container_start_page | 3903 |
container_title | Earthquake engineering & structural dynamics |
container_volume | 52 |
creator | Baltzopoulos, Georgios Baraschino, Roberto Chioccarelli, Eugenio Cito, Pasquale Vitale, Antonio Iervolino, Iunio |
description | On the night of February 6, 2023, a major earthquake struck Turkey and nearby Syria, whose moment magnitude (M) was estimated at 7.8 (or 7.7, depending on the data source). It started what can be considered a seismic sequence with thousands of recorded earthquakes with magnitude larger than two, including another M6.7 event (or 6.6) occurring shortly after, and one M7.5 (or 7.6) a day and a half later. The area in the south‐eastern part of Turkey hit by the sequence is considered, according to probabilistic models, one of the most hazardous in the wider region. This technical note aims at a preliminary illustration of some features of the shaking, deemed of earthquake engineering relevance. To this aim, it preliminarily analyzes the evolution of the sequence so far and the related ground motion intensity, as estimated from ShakeMap envelopes, then focuses on the largest magnitude event, for which a preliminary model of the source is available, while a supplementary report is provided for the other two events. Based on data available at the time of writing, it is found that the development of the sequence and the recorded ground motions are generally in agreement with available models, although some locations may have experienced peak ground accelerations larger than 1.0 g, and near‐source effects, determining pulse‐like ground motions, apparently occurred. |
doi_str_mv | 10.1002/eqe.3939 |
format | article |
fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_2859553550</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2859553550</sourcerecordid><originalsourceid>FETCH-LOGICAL-c3279-c8aff7a9cfbfebaba8b93c0f61c0770ac594859a51c43f091514ac4725ccd1253</originalsourceid><addsrcrecordid>eNp10E1OwzAQBWALgUQpSBzBEpuySBnHcW0vURUKUgEhlbXluDZNf5LWToTCiiNwRk6CS9myms33ZkYPoUsCQwKQ3tidHVJJ5RHqEZCjRIqMHaMegBSJEBk_RWchLAGAjoD3UP5ktf_-_Ap1643Fb75uqzne1E1ZV7iscLOw-JEPBZ7oj1JXjd3iwaz1K9td45hsFrtWr-w5OnF6HezF3-yj17t8Nr5Pps-Th_HtNDE05TIxQjvHtTSucLbQhRaFpAbciBjgHLRhMhNMakZMRh1IwkimTcZTZsycpIz20dVh79bXu9aGRi3j31U8qdIYZIwyBlENDsr4OgRvndr6cqN9pwiofUkqlqT2JUWaHOh7ubbdv07lL_mv_wETRGgt</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2859553550</pqid></control><display><type>article</type><title>Near‐source ground motion in the M7.8 Gaziantep (Turkey) earthquake</title><source>Wiley-Blackwell Read & Publish Collection</source><creator>Baltzopoulos, Georgios ; Baraschino, Roberto ; Chioccarelli, Eugenio ; Cito, Pasquale ; Vitale, Antonio ; Iervolino, Iunio</creator><creatorcontrib>Baltzopoulos, Georgios ; Baraschino, Roberto ; Chioccarelli, Eugenio ; Cito, Pasquale ; Vitale, Antonio ; Iervolino, Iunio</creatorcontrib><description>On the night of February 6, 2023, a major earthquake struck Turkey and nearby Syria, whose moment magnitude (M) was estimated at 7.8 (or 7.7, depending on the data source). It started what can be considered a seismic sequence with thousands of recorded earthquakes with magnitude larger than two, including another M6.7 event (or 6.6) occurring shortly after, and one M7.5 (or 7.6) a day and a half later. The area in the south‐eastern part of Turkey hit by the sequence is considered, according to probabilistic models, one of the most hazardous in the wider region. This technical note aims at a preliminary illustration of some features of the shaking, deemed of earthquake engineering relevance. To this aim, it preliminarily analyzes the evolution of the sequence so far and the related ground motion intensity, as estimated from ShakeMap envelopes, then focuses on the largest magnitude event, for which a preliminary model of the source is available, while a supplementary report is provided for the other two events. Based on data available at the time of writing, it is found that the development of the sequence and the recorded ground motions are generally in agreement with available models, although some locations may have experienced peak ground accelerations larger than 1.0 g, and near‐source effects, determining pulse‐like ground motions, apparently occurred.</description><identifier>ISSN: 0098-8847</identifier><identifier>EISSN: 1096-9845</identifier><identifier>DOI: 10.1002/eqe.3939</identifier><language>eng</language><publisher>Bognor Regis: Wiley Subscription Services, Inc</publisher><subject>aftershock sequence ; earthquake data ; Earthquake engineering ; Earthquakes ; Ground motion ; Illustrations ; Mathematical models ; Probabilistic models ; pulse‐like ground motions ; response spectra ; Seismic activity ; Seismic engineering ; Sequencing ; Shaking</subject><ispartof>Earthquake engineering & structural dynamics, 2023-10, Vol.52 (12), p.3903-3912</ispartof><rights>2023 The Authors. published by John Wiley & Sons Ltd.</rights><rights>2023. This article is published under http://creativecommons.org/licenses/by-nc-nd/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c3279-c8aff7a9cfbfebaba8b93c0f61c0770ac594859a51c43f091514ac4725ccd1253</citedby><cites>FETCH-LOGICAL-c3279-c8aff7a9cfbfebaba8b93c0f61c0770ac594859a51c43f091514ac4725ccd1253</cites><orcidid>0000-0002-8363-9306 ; 0000-0001-6603-8106 ; 0000-0002-0460-6558 ; 0000-0002-8990-3120 ; 0000-0002-4076-2718</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,777,781,27905,27906</link.rule.ids></links><search><creatorcontrib>Baltzopoulos, Georgios</creatorcontrib><creatorcontrib>Baraschino, Roberto</creatorcontrib><creatorcontrib>Chioccarelli, Eugenio</creatorcontrib><creatorcontrib>Cito, Pasquale</creatorcontrib><creatorcontrib>Vitale, Antonio</creatorcontrib><creatorcontrib>Iervolino, Iunio</creatorcontrib><title>Near‐source ground motion in the M7.8 Gaziantep (Turkey) earthquake</title><title>Earthquake engineering & structural dynamics</title><description>On the night of February 6, 2023, a major earthquake struck Turkey and nearby Syria, whose moment magnitude (M) was estimated at 7.8 (or 7.7, depending on the data source). It started what can be considered a seismic sequence with thousands of recorded earthquakes with magnitude larger than two, including another M6.7 event (or 6.6) occurring shortly after, and one M7.5 (or 7.6) a day and a half later. The area in the south‐eastern part of Turkey hit by the sequence is considered, according to probabilistic models, one of the most hazardous in the wider region. This technical note aims at a preliminary illustration of some features of the shaking, deemed of earthquake engineering relevance. To this aim, it preliminarily analyzes the evolution of the sequence so far and the related ground motion intensity, as estimated from ShakeMap envelopes, then focuses on the largest magnitude event, for which a preliminary model of the source is available, while a supplementary report is provided for the other two events. Based on data available at the time of writing, it is found that the development of the sequence and the recorded ground motions are generally in agreement with available models, although some locations may have experienced peak ground accelerations larger than 1.0 g, and near‐source effects, determining pulse‐like ground motions, apparently occurred.</description><subject>aftershock sequence</subject><subject>earthquake data</subject><subject>Earthquake engineering</subject><subject>Earthquakes</subject><subject>Ground motion</subject><subject>Illustrations</subject><subject>Mathematical models</subject><subject>Probabilistic models</subject><subject>pulse‐like ground motions</subject><subject>response spectra</subject><subject>Seismic activity</subject><subject>Seismic engineering</subject><subject>Sequencing</subject><subject>Shaking</subject><issn>0098-8847</issn><issn>1096-9845</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><sourceid>24P</sourceid><recordid>eNp10E1OwzAQBWALgUQpSBzBEpuySBnHcW0vURUKUgEhlbXluDZNf5LWToTCiiNwRk6CS9myms33ZkYPoUsCQwKQ3tidHVJJ5RHqEZCjRIqMHaMegBSJEBk_RWchLAGAjoD3UP5ktf_-_Ap1643Fb75uqzne1E1ZV7iscLOw-JEPBZ7oj1JXjd3iwaz1K9td45hsFrtWr-w5OnF6HezF3-yj17t8Nr5Pps-Th_HtNDE05TIxQjvHtTSucLbQhRaFpAbciBjgHLRhMhNMakZMRh1IwkimTcZTZsycpIz20dVh79bXu9aGRi3j31U8qdIYZIwyBlENDsr4OgRvndr6cqN9pwiofUkqlqT2JUWaHOh7ubbdv07lL_mv_wETRGgt</recordid><startdate>20231001</startdate><enddate>20231001</enddate><creator>Baltzopoulos, Georgios</creator><creator>Baraschino, Roberto</creator><creator>Chioccarelli, Eugenio</creator><creator>Cito, Pasquale</creator><creator>Vitale, Antonio</creator><creator>Iervolino, Iunio</creator><general>Wiley Subscription Services, Inc</general><scope>24P</scope><scope>WIN</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7ST</scope><scope>7TG</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H96</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>SOI</scope><orcidid>https://orcid.org/0000-0002-8363-9306</orcidid><orcidid>https://orcid.org/0000-0001-6603-8106</orcidid><orcidid>https://orcid.org/0000-0002-0460-6558</orcidid><orcidid>https://orcid.org/0000-0002-8990-3120</orcidid><orcidid>https://orcid.org/0000-0002-4076-2718</orcidid></search><sort><creationdate>20231001</creationdate><title>Near‐source ground motion in the M7.8 Gaziantep (Turkey) earthquake</title><author>Baltzopoulos, Georgios ; Baraschino, Roberto ; Chioccarelli, Eugenio ; Cito, Pasquale ; Vitale, Antonio ; Iervolino, Iunio</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3279-c8aff7a9cfbfebaba8b93c0f61c0770ac594859a51c43f091514ac4725ccd1253</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>aftershock sequence</topic><topic>earthquake data</topic><topic>Earthquake engineering</topic><topic>Earthquakes</topic><topic>Ground motion</topic><topic>Illustrations</topic><topic>Mathematical models</topic><topic>Probabilistic models</topic><topic>pulse‐like ground motions</topic><topic>response spectra</topic><topic>Seismic activity</topic><topic>Seismic engineering</topic><topic>Sequencing</topic><topic>Shaking</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Baltzopoulos, Georgios</creatorcontrib><creatorcontrib>Baraschino, Roberto</creatorcontrib><creatorcontrib>Chioccarelli, Eugenio</creatorcontrib><creatorcontrib>Cito, Pasquale</creatorcontrib><creatorcontrib>Vitale, Antonio</creatorcontrib><creatorcontrib>Iervolino, Iunio</creatorcontrib><collection>Wiley Open Access</collection><collection>Wiley Online Library Open Access</collection><collection>CrossRef</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Environment Abstracts</collection><jtitle>Earthquake engineering & structural dynamics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Baltzopoulos, Georgios</au><au>Baraschino, Roberto</au><au>Chioccarelli, Eugenio</au><au>Cito, Pasquale</au><au>Vitale, Antonio</au><au>Iervolino, Iunio</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Near‐source ground motion in the M7.8 Gaziantep (Turkey) earthquake</atitle><jtitle>Earthquake engineering & structural dynamics</jtitle><date>2023-10-01</date><risdate>2023</risdate><volume>52</volume><issue>12</issue><spage>3903</spage><epage>3912</epage><pages>3903-3912</pages><issn>0098-8847</issn><eissn>1096-9845</eissn><abstract>On the night of February 6, 2023, a major earthquake struck Turkey and nearby Syria, whose moment magnitude (M) was estimated at 7.8 (or 7.7, depending on the data source). It started what can be considered a seismic sequence with thousands of recorded earthquakes with magnitude larger than two, including another M6.7 event (or 6.6) occurring shortly after, and one M7.5 (or 7.6) a day and a half later. The area in the south‐eastern part of Turkey hit by the sequence is considered, according to probabilistic models, one of the most hazardous in the wider region. This technical note aims at a preliminary illustration of some features of the shaking, deemed of earthquake engineering relevance. To this aim, it preliminarily analyzes the evolution of the sequence so far and the related ground motion intensity, as estimated from ShakeMap envelopes, then focuses on the largest magnitude event, for which a preliminary model of the source is available, while a supplementary report is provided for the other two events. Based on data available at the time of writing, it is found that the development of the sequence and the recorded ground motions are generally in agreement with available models, although some locations may have experienced peak ground accelerations larger than 1.0 g, and near‐source effects, determining pulse‐like ground motions, apparently occurred.</abstract><cop>Bognor Regis</cop><pub>Wiley Subscription Services, Inc</pub><doi>10.1002/eqe.3939</doi><tpages>10</tpages><orcidid>https://orcid.org/0000-0002-8363-9306</orcidid><orcidid>https://orcid.org/0000-0001-6603-8106</orcidid><orcidid>https://orcid.org/0000-0002-0460-6558</orcidid><orcidid>https://orcid.org/0000-0002-8990-3120</orcidid><orcidid>https://orcid.org/0000-0002-4076-2718</orcidid><oa>free_for_read</oa></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0098-8847 |
ispartof | Earthquake engineering & structural dynamics, 2023-10, Vol.52 (12), p.3903-3912 |
issn | 0098-8847 1096-9845 |
language | eng |
recordid | cdi_proquest_journals_2859553550 |
source | Wiley-Blackwell Read & Publish Collection |
subjects | aftershock sequence earthquake data Earthquake engineering Earthquakes Ground motion Illustrations Mathematical models Probabilistic models pulse‐like ground motions response spectra Seismic activity Seismic engineering Sequencing Shaking |
title | Near‐source ground motion in the M7.8 Gaziantep (Turkey) earthquake |
url | http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-19T20%3A59%3A43IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Near%E2%80%90source%20ground%20motion%20in%20the%20M7.8%20Gaziantep%20(Turkey)%20earthquake&rft.jtitle=Earthquake%20engineering%20&%20structural%20dynamics&rft.au=Baltzopoulos,%20Georgios&rft.date=2023-10-01&rft.volume=52&rft.issue=12&rft.spage=3903&rft.epage=3912&rft.pages=3903-3912&rft.issn=0098-8847&rft.eissn=1096-9845&rft_id=info:doi/10.1002/eqe.3939&rft_dat=%3Cproquest_cross%3E2859553550%3C/proquest_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c3279-c8aff7a9cfbfebaba8b93c0f61c0770ac594859a51c43f091514ac4725ccd1253%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=2859553550&rft_id=info:pmid/&rfr_iscdi=true |