Dense Seismic Recordings of the 2023 KahramanmaraşEarthquake Sequence in Southeastern Türkiye

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Özet

The devastating 6 February 2023 Kahramanmara & scedil;earthquake sequence in southeastern T & uuml;rkiye started with a moment magnitude (Mw) 7.8 earthquake, for which the initial rupture broke the Sak4ag & ouml;z segment near Nurda & gbreve;& imath; and then jumped into a bilateral rupture along multiple segments of the Eastern Anatolian fault zone (EAFZ). This complicated rupture was followed nine hours later by an Mw 7.6 event near Ekin & ouml;z & uuml;. To better understand the spatiotemporal evolution of aftershocks, site amplification, and the structural and tectonic framework of the EAFZ in this diffuse triple junction, we deployed a dense seismometer array covering both aftershock zones for nearly four months. The main Eastern Anatolian Seismic Temporary (EAST) array includes 125 nodal, 10 broadband, and 6 strong-motion seismic stations distributed around the rupture zone. An additional linear array of 73 nodal stations was also installed across the Pazarc & imath;k segment of the EAFZ and the Sak4ag & ouml;z segment near the Mw 7.8 epicenter to record fault-zone waves for similar to 30 days. This article shows example recordings and the EAST array geometry, preliminary research results, and the metadata related to all of the stations in this array. A deep-learning-based phase picking for one month of continuous recording yielded millions of seismic phase readings and tens of thousands of aftershock locations after phase associations. We also give examples of both local and teleseismic waveforms recorded by the nodal arrays, which can be used for subsequent high-resolution earthquake relocation, imaging of crustal structures, and fault-zone imaging.

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https://doi.org/10.1785/0220240152Yayıncı resmi DOI adresi
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AlanDeğerDil
dc.contributor.authorZor, Ekrem
dc.contributor.authorPeng, Zhigang
dc.contributor.authorErgin, Mehmet
dc.contributor.authorSandvol, Eric
dc.contributor.authorSevim, Fatih
dc.contributor.authorRdamaz, Mustafa Cengiz Tap i
dc.contributor.authorMach, Phuc
dc.contributor.authorYalvac, Ouzhan
dc.contributor.authorTarancioglu, Adil
dc.contributor.authorAdeboboye, Oluwaseyifunmi
dc.contributor.authorDing, Chang
dc.contributor.authorAcikgoez, Cem
dc.contributor.authorBueyuek, Ersin
dc.date.accessioned2026-10-22T09:23:04.056467337Z
dc.date.available2026-10-22T09:23:04.056467337Z
dc.date.issued2025-07
dc.description.abstractThe devastating 6 February 2023 Kahramanmara & scedil;earthquake sequence in southeastern T & uuml;rkiye started with a moment magnitude (Mw) 7.8 earthquake, for which the initial rupture broke the Sak4ag & ouml;z segment near Nurda & gbreve;& imath; and then jumped into a bilateral rupture along multiple segments of the Eastern Anatolian fault zone (EAFZ). This complicated rupture was followed nine hours later by an Mw 7.6 event near Ekin & ouml;z & uuml;. To better understand the spatiotemporal evolution of aftershocks, site amplification, and the structural and tectonic framework of the EAFZ in this diffuse triple junction, we deployed a dense seismometer array covering both aftershock zones for nearly four months. The main Eastern Anatolian Seismic Temporary (EAST) array includes 125 nodal, 10 broadband, and 6 strong-motion seismic stations distributed around the rupture zone. An additional linear array of 73 nodal stations was also installed across the Pazarc & imath;k segment of the EAFZ and the Sak4ag & ouml;z segment near the Mw 7.8 epicenter to record fault-zone waves for similar to 30 days. This article shows example recordings and the EAST array geometry, preliminary research results, and the metadata related to all of the stations in this array. A deep-learning-based phase picking for one month of continuous recording yielded millions of seismic phase readings and tens of thousands of aftershock locations after phase associations. We also give examples of both local and teleseismic waveforms recorded by the nodal arrays, which can be used for subsequent high-resolution earthquake relocation, imaging of crustal structures, and fault-zone imaging.
dc.description.sponsorshipU.S. National Science Foundation (NSF)' s Rapid Response Research (RAPID) Grant [EAR-2322460]
dc.description.sponsorshipNSF RAPID Grant [EAR-232246]
dc.description.sponsorshipTUBITAK Marmara Research Center's Internal Aftershock Project [5207901]
dc.identifier.doi10.1785/0220240152
dc.identifier.eissn1938-2057
dc.identifier.endpage2697
dc.identifier.issn0895-0695
dc.identifier.issue4
dc.identifier.scopus2-s2.0-105009946111
dc.identifier.startpage2683
dc.identifier.urihttps://rdlopen.rawdatalibrary.net/r/gumushane/10535
dc.identifier.volume96
dc.identifier.wosWOS:001533699100046
dc.language.isoen
dc.publisherSEISMOLOGICAL SOC AMER
dc.relation.ispartofSEISMOLOGICAL RESEARCH LETTERS
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.subject.classificationGeochemistry & Geophysics
dc.subject.otherSAN-JACINTO FAULT
dc.subject.otherSINGLE-STATION MICROTREMOR
dc.subject.otherEAST ANATOLIAN FAULT
dc.subject.otherAMBIENT NOISE-LEVELS
dc.subject.otherBAY AREA TURKEY
dc.subject.otherEARTHQUAKE SEQUENCE
dc.subject.otherSPECTRAL RATIO
dc.subject.otherTRAPPED WAVES
dc.subject.otherZONE
dc.subject.otherARRAY
dc.titleDense Seismic Recordings of the 2023 KahramanmaraşEarthquake Sequence in Southeastern Türkiye
dc.typeArticle
rdl.citation.openalex7
rdl.citation.scopus5
rdl.citation.wos5
rdl.oa.statusclosed
rdl.scopus.quartileQ1
rdl.source.indexWOS
rdl.source.indexSCOPUS
rdl.wos.indexScience Citation Index Expanded (SCI-EXPANDED)