Preliminary report of coseismic surface rupture (part) of Türkiye's MW7.8 earthquake by remote sensing interpretation

Both MW 7.8 and MW 7.5 earthquakes occurred in southeastern Türkiye on February 6, 2023, resulting in numerous buildings collapsing and serious casualties. Understanding the distribution of coseismic surface ruptures and secondary disasters surrounding the epicentral area is important for post-earth...

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Main Authors: Yali Guo, Haofeng Li, Peng Liang, Renwei Xiong, Chaozhong Hu, Yueren Xu
Format: Article
Language:English
Published: KeAi Communications Co. Ltd. 2024-01-01
Series:Earthquake Research Advances
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S2772467023000167
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author Yali Guo
Haofeng Li
Peng Liang
Renwei Xiong
Chaozhong Hu
Yueren Xu
author_facet Yali Guo
Haofeng Li
Peng Liang
Renwei Xiong
Chaozhong Hu
Yueren Xu
author_sort Yali Guo
collection DOAJ
description Both MW 7.8 and MW 7.5 earthquakes occurred in southeastern Türkiye on February 6, 2023, resulting in numerous buildings collapsing and serious casualties. Understanding the distribution of coseismic surface ruptures and secondary disasters surrounding the epicentral area is important for post-earthquake emergency and disaster assessments. High-resolution Maxar and GF-2 satellite data were used after the events to extract the location of the rupture surrounding the first epicentral area. The results show that the length of the interpreted surface rupture zone (part of) is approximately 75 ​km, with a coseismic sinistral dislocation of 2–3 ​m near the epicenter; however, this reduced to zero at the tip of the southwest section of the East Anatolia Fault Zone. Moreover, dense soil liquefaction pits were triggered along the rupture trace. These events are in the western region of the Eurasian Seismic Belt and result from the subduction and collision of the Arabian and African Plates toward the Eurasian Plate. The western region of Chinese mainland and its adjacent areas are in the eastern section of the Eurasian Seismic Belt, where seismic activity is controlled by the collision of the Indian and Eurasian Plates. Both China and Türkiye have independent tectonic histories.
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spelling doaj.art-ca0e27ebaa6f4ae589bbc4dd66e85d242024-01-31T05:45:54ZengKeAi Communications Co. Ltd.Earthquake Research Advances2772-46702024-01-0141100219Preliminary report of coseismic surface rupture (part) of Türkiye's MW7.8 earthquake by remote sensing interpretationYali Guo0Haofeng Li1Peng Liang2Renwei Xiong3Chaozhong Hu4Yueren Xu5Key Laboratory of Earthquake Prediction, Institute of Earthquake Forecasting, China Earthquake Administration, Beijing, 100036, ChinaKey Laboratory of Earthquake Prediction, Institute of Earthquake Forecasting, China Earthquake Administration, Beijing, 100036, ChinaCorresponding author.; Key Laboratory of Earthquake Prediction, Institute of Earthquake Forecasting, China Earthquake Administration, Beijing, 100036, ChinaKey Laboratory of Earthquake Prediction, Institute of Earthquake Forecasting, China Earthquake Administration, Beijing, 100036, ChinaKey Laboratory of Earthquake Prediction, Institute of Earthquake Forecasting, China Earthquake Administration, Beijing, 100036, ChinaCorresponding author.; Key Laboratory of Earthquake Prediction, Institute of Earthquake Forecasting, China Earthquake Administration, Beijing, 100036, ChinaBoth MW 7.8 and MW 7.5 earthquakes occurred in southeastern Türkiye on February 6, 2023, resulting in numerous buildings collapsing and serious casualties. Understanding the distribution of coseismic surface ruptures and secondary disasters surrounding the epicentral area is important for post-earthquake emergency and disaster assessments. High-resolution Maxar and GF-2 satellite data were used after the events to extract the location of the rupture surrounding the first epicentral area. The results show that the length of the interpreted surface rupture zone (part of) is approximately 75 ​km, with a coseismic sinistral dislocation of 2–3 ​m near the epicenter; however, this reduced to zero at the tip of the southwest section of the East Anatolia Fault Zone. Moreover, dense soil liquefaction pits were triggered along the rupture trace. These events are in the western region of the Eurasian Seismic Belt and result from the subduction and collision of the Arabian and African Plates toward the Eurasian Plate. The western region of Chinese mainland and its adjacent areas are in the eastern section of the Eurasian Seismic Belt, where seismic activity is controlled by the collision of the Indian and Eurasian Plates. Both China and Türkiye have independent tectonic histories.http://www.sciencedirect.com/science/article/pii/S27724670230001672023 Türkiye Mw7.8 earthquakeCoseismic surface ruptureEast anatolian fault zoneEurasian seismic zoneRemote sensing interpretation
spellingShingle Yali Guo
Haofeng Li
Peng Liang
Renwei Xiong
Chaozhong Hu
Yueren Xu
Preliminary report of coseismic surface rupture (part) of Türkiye's MW7.8 earthquake by remote sensing interpretation
Earthquake Research Advances
2023 Türkiye Mw7.8 earthquake
Coseismic surface rupture
East anatolian fault zone
Eurasian seismic zone
Remote sensing interpretation
title Preliminary report of coseismic surface rupture (part) of Türkiye's MW7.8 earthquake by remote sensing interpretation
title_full Preliminary report of coseismic surface rupture (part) of Türkiye's MW7.8 earthquake by remote sensing interpretation
title_fullStr Preliminary report of coseismic surface rupture (part) of Türkiye's MW7.8 earthquake by remote sensing interpretation
title_full_unstemmed Preliminary report of coseismic surface rupture (part) of Türkiye's MW7.8 earthquake by remote sensing interpretation
title_short Preliminary report of coseismic surface rupture (part) of Türkiye's MW7.8 earthquake by remote sensing interpretation
title_sort preliminary report of coseismic surface rupture part of turkiye s mw7 8 earthquake by remote sensing interpretation
topic 2023 Türkiye Mw7.8 earthquake
Coseismic surface rupture
East anatolian fault zone
Eurasian seismic zone
Remote sensing interpretation
url http://www.sciencedirect.com/science/article/pii/S2772467023000167
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