3D Coseismic Deformation and Fault Slip Model of the 2023 Kahramanmara?Earthquake Sequence Constrained by GPS,ALOS-2 and Sentinel-1 Data  

作　　者：Chengyuan Bai Wenbin Xu Lei Zhao Kai Sun Lei Xie 

机构地区：[1]School of Geosciences and Info-Physics,Central South University,Changsha 410083,China

出　　处：《Journal of Earth Science》2025年第2期812-822,共11页地球科学学刊(英文版)

基　　金：supported by the National Natural Science Foundation of China(Nos.42174023,42304037);the National Key Research and Development Program(No.2022YFB3903602);the Natural Science Foundation of Hunan Province(No.2024JJ3031);the Frontier Cross Research Project of Central South University(No.2023QYJC006)。

摘　　要：0 INTRODUCTION Turkey is located at the intersection of the Eurasian,Anatolian,Arabian,and African tectonic plates.Due to the ongoing northward compression from the Arabian Plate,the Anatolian Plate is pushed westward in a tectonic escape mechanism,leading to the formation of the North Anatolian fault zone(NAFZ)and the East Anatolian fault zone(EAFZ)(e.g.,Bayrak et al.,2015;Duman and Emre,2013;Reilinger et al.,2006).

关 键 词：north anatolian fault zone nafz fault slip ALOS coseismic deformation kahramanmara earthquake GPS SENTINEL anatolian plate 

分 类 号：P315.7[天文地球—地震学]