|国家科技期刊平台
首页|期刊导航|地震研究进展(英文)|Preliminary report of coseismic surface rupture(part)of Türkiye's MW7.8 earthquake by remote sensing interpretation

Preliminary report of coseismic surface rupture(part)of Türkiye's MW7.8 earthquake by remote sensing interpretationOA北大核心

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

英文摘要

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 rup-tures 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 the 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.

Yali Guo;Haofeng Li;Peng Liang;Renwei Xiong;Chaozhong Hu;Yueren Xu

Key Laboratory of Earthquake Prediction,Institute of Earthquake Forecasting,China Earthquake Administration,Beijing,100036,China

2023 Türkiye MW7.8 earthquakeCoseismic surface ruptureEast anatolian fault zoneEurasian seismic zoneRemote sensing interpretation

《地震研究进展(英文)》 2024 (001)

4-13 / 10

This research was funded by the Basic Research Program of the Institute of Earthquake Forecasting,China Earthquake Administration(Grant Nos.CEAIEF20220102,2021IEF0505,and CEAIEF2022050502),the National Natural Science Foundation of China(Grant Nos.42072248 and 42041006),and the National Key Research and Development Pro-gram of China(Grant Nos.2021YFC3000601-3 and 2019YFE0108900).We would like to thank Editage(www.editage.cn)for English language editing.

10.1016/j.eqrea.2023.100219

评论