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      The preparatory process of the 2023 Mw 7.8 Türkiye earthquake

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          Abstract

          To verify the existence of a preparatory process for the 6 February 2023, Mw 7.8 Kahramanmaraş earthquake, southern Türkiye, we analyze the temporal evolution of seismic catalog information for ~ 7500 earthquakes with magnitudes M L ≥ 1.5, which occurred along the main segments of the East Anatolian Fault (EAF) since 2014. We find the EAF fault segments showing different temporal patterns in the proportion of nonclustered seismicity, which we interpret as temporal variation of coupling. We also study the evolution of the b-value, fractal dimension and energy rate. These seismic features show for the Amanos and Pazarcık fault segments a long-term trend during the period 2020–2022 that might correspond to a quiescence phase. The latter is followed by a change in earthquakes clustering and characteristics that starts about eight months before the Mw 7.8 Kahramanmaraş event. Our observations confirm the existence of a long-lasting preparatory phase for the 2023, Mw 7.8 Kahramanmaraş earthquake and can stimulate new investigations on the East Anatolian Fault mechanic. Intercepting when a fault starts deviating from its steady behavior, might be the key for identifying the preparatory phase of large earthquakes and mitigate seismic risk.

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          Characterization of Strange Attractors

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            Bootstrap Methods: Another Look at the Jackknife

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              Propagation of slow slip leading up to the 2011 M(w) 9.0 Tohoku-Oki earthquake.

              Many large earthquakes are preceded by one or more foreshocks, but it is unclear how these foreshocks relate to the nucleation process of the mainshock. On the basis of an earthquake catalog created using a waveform correlation technique, we identified two distinct sequences of foreshocks migrating at rates of 2 to 10 kilometers per day along the trench axis toward the epicenter of the 2011 moment magnitude (M(w)) 9.0 Tohoku-Oki earthquake in Japan. The time history of quasi-static slip along the plate interface, based on small repeating earthquakes that were part of the migrating seismicity, suggests that two sequences involved slow-slip transients propagating toward the initial rupture point. The second sequence, which involved large slip rates, may have caused substantial stress loading, prompting the unstable dynamic rupture of the mainshock.
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                Author and article information

                Contributors
                matteo.picozzi@unina.it
                Journal
                Sci Rep
                Sci Rep
                Scientific Reports
                Nature Publishing Group UK (London )
                2045-2322
                19 October 2023
                19 October 2023
                2023
                : 13
                : 17853
                Affiliations
                [1 ]University of Naples Federico II, ( https://ror.org/05290cv24) Naples, Italy
                [2 ]DISTAV, University of Genoa, ( https://ror.org/0107c5v14) Genoa, Italy
                Article
                45073
                10.1038/s41598-023-45073-8
                10587168
                37857660
                6316e1b2-4ae9-4714-8411-261561324d28
                © Springer Nature Limited 2023

                Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.

                History
                : 19 May 2023
                : 16 October 2023
                Funding
                Funded by: PRIN 2022 project ’2022ZHXWC9’ - Intercepting the PREparatory Phase of lARge earthquakes from seismic information and gEodetic Displacement (PREPARED).
                Funded by: Program STAR PLUS by University of Naples Federico II and Compagnia di San Paolo.
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                © Springer Nature Limited 2023

                Uncategorized
                seismology,natural hazards
                Uncategorized
                seismology, natural hazards

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