{"title":"2023年2月6日土耳其地震前地震活动的RTL异常","authors":"V. B. Smirnov, A. A. Petrushov, V. O. Mikhailov","doi":"10.1134/S1069351323060204","DOIUrl":null,"url":null,"abstract":"<div><div><p><b>Abstract</b>—Based on the data from the regional Turkey earthquake catalog and the ANSS Comprehensive Earthquake Catalog for Turkey and a part of Iran, a posteriori analysis of RTL anomalies of seismicity before the damaging <i>M</i><sub><i>w</i></sub> 7.8 Pazarcik earthquake in Turkey of February 6, 2023 and, for comparison, before the <i>M</i><sub><i>w</i></sub> 7.1 earthquake of October 23, 2011 (Eastern Turkey), the <i>M</i><sub><i>w</i></sub> 7.3 earthquake of November 12, 2017 (Iran), and the <i>М</i> 6.7 earthquake of January 24, 2020 (the East Anatolian Fault), was made. Distinctly observable before the Pazarcik earthquake is an RTL anomaly with well-marked stages of a seismic quiescence and subsequent activation near the epicenter of the future earthquake. Spatially, the anomaly is one-and-a-half times smaller than the source of the Pazarcik earthquake, and one-and-a-half—two times smaller than RTL anomalies before other regional earthquakes with a magnitude above 7. By size, it corresponds to the anomaly before the <i>M</i><sub><i>w</i></sub> 6.7 earthquake that occurred on the same fault. As a hypothesis to explain why the size of the anomaly before the <i>M</i><sub><i>w</i></sub> 7.8 Pazarcik earthquake does not match the sizes of the anomalies characteristic of <i>M</i>7+ earthquakes, it was assumed that the detected RTL anomaly reflects the formation only of the first, relatively small segment of the source of the Pazarcik earthquake.</p></div></div>","PeriodicalId":602,"journal":{"name":"Izvestiya, Physics of the Solid Earth","volume":"59 6","pages":"929 - 938"},"PeriodicalIF":0.9000,"publicationDate":"2023-11-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"The RTL Anomaly of Seismicity before the February 6, 2023 Earthquake in Turkey\",\"authors\":\"V. B. Smirnov, A. A. Petrushov, V. O. Mikhailov\",\"doi\":\"10.1134/S1069351323060204\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div><p><b>Abstract</b>—Based on the data from the regional Turkey earthquake catalog and the ANSS Comprehensive Earthquake Catalog for Turkey and a part of Iran, a posteriori analysis of RTL anomalies of seismicity before the damaging <i>M</i><sub><i>w</i></sub> 7.8 Pazarcik earthquake in Turkey of February 6, 2023 and, for comparison, before the <i>M</i><sub><i>w</i></sub> 7.1 earthquake of October 23, 2011 (Eastern Turkey), the <i>M</i><sub><i>w</i></sub> 7.3 earthquake of November 12, 2017 (Iran), and the <i>М</i> 6.7 earthquake of January 24, 2020 (the East Anatolian Fault), was made. Distinctly observable before the Pazarcik earthquake is an RTL anomaly with well-marked stages of a seismic quiescence and subsequent activation near the epicenter of the future earthquake. Spatially, the anomaly is one-and-a-half times smaller than the source of the Pazarcik earthquake, and one-and-a-half—two times smaller than RTL anomalies before other regional earthquakes with a magnitude above 7. By size, it corresponds to the anomaly before the <i>M</i><sub><i>w</i></sub> 6.7 earthquake that occurred on the same fault. As a hypothesis to explain why the size of the anomaly before the <i>M</i><sub><i>w</i></sub> 7.8 Pazarcik earthquake does not match the sizes of the anomalies characteristic of <i>M</i>7+ earthquakes, it was assumed that the detected RTL anomaly reflects the formation only of the first, relatively small segment of the source of the Pazarcik earthquake.</p></div></div>\",\"PeriodicalId\":602,\"journal\":{\"name\":\"Izvestiya, Physics of the Solid Earth\",\"volume\":\"59 6\",\"pages\":\"929 - 938\"},\"PeriodicalIF\":0.9000,\"publicationDate\":\"2023-11-28\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Izvestiya, Physics of the Solid Earth\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://link.springer.com/article/10.1134/S1069351323060204\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Izvestiya, Physics of the Solid Earth","FirstCategoryId":"89","ListUrlMain":"https://link.springer.com/article/10.1134/S1069351323060204","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
The RTL Anomaly of Seismicity before the February 6, 2023 Earthquake in Turkey
Abstract—Based on the data from the regional Turkey earthquake catalog and the ANSS Comprehensive Earthquake Catalog for Turkey and a part of Iran, a posteriori analysis of RTL anomalies of seismicity before the damaging Mw 7.8 Pazarcik earthquake in Turkey of February 6, 2023 and, for comparison, before the Mw 7.1 earthquake of October 23, 2011 (Eastern Turkey), the Mw 7.3 earthquake of November 12, 2017 (Iran), and the М 6.7 earthquake of January 24, 2020 (the East Anatolian Fault), was made. Distinctly observable before the Pazarcik earthquake is an RTL anomaly with well-marked stages of a seismic quiescence and subsequent activation near the epicenter of the future earthquake. Spatially, the anomaly is one-and-a-half times smaller than the source of the Pazarcik earthquake, and one-and-a-half—two times smaller than RTL anomalies before other regional earthquakes with a magnitude above 7. By size, it corresponds to the anomaly before the Mw 6.7 earthquake that occurred on the same fault. As a hypothesis to explain why the size of the anomaly before the Mw 7.8 Pazarcik earthquake does not match the sizes of the anomalies characteristic of M7+ earthquakes, it was assumed that the detected RTL anomaly reflects the formation only of the first, relatively small segment of the source of the Pazarcik earthquake.
期刊介绍:
Izvestiya, Physics of the Solid Earth is an international peer reviewed journal that publishes results of original theoretical and experimental research in relevant areas of the physics of the Earth''s interior and applied geophysics. The journal welcomes manuscripts from all countries in the English or Russian language.