Lithospheric strength of the Anatolian plateau and implications for strong earthquake activity in TurkeyOAEI
Lithospheric strength of the Anatolian plateau and implications for strong earthquake activity in Turkey
On February 6,2023,the doublet earthquake including two main shocks with magnitudes Mw7.8 and Mw7.5,occurred near the western side of the East Anatolian Fault at the southeast boundary of the Anatolian Plateau in Turkey.Based on the WGM2012 Bouguer gravity anomaly data and the Etopo1 topography data,this study first introduced a joint inversion of admittance and coherence functions and used the Bayesian optimal parameter estimation method to obtain the effective elastic thickness Te and loading ratio F of the lithosphere for various tectonic units in the Anatolian Plateau.Secondly,we dis-cussed the characteristics and influencing factors of the lithospheric mechanical strength and analyzed its relationship with seismic activity.The lithospheric mechanical strength of the Anatolian Plateau showed clear lateral heterogeneity and a"weak-strong-weak"spatial pattern from east to west,reflecting various tectonic processes.At last,the strong seismic activity was found where the lithospheric strength was low in the Anatolian Plate.We also incorporated GPS strain rate and other results to investigate the tectonic background and primary causes of the Mw7.8 and Mw7.5 doublet earthquakes in Turkey.The results have a good insight into urban safety design in the Turkish region,including post-disaster rehabilitation,earthquake hazard assessment,and loss reduction.
Yuhang Pan;Shi Chen;Wen Shi
Institute of Geophysics,China Earthquake Administration,Beijing 100081,China||Beijing Baijiatuan Earth Science National Observation and Research Station,Beijing 100095,China
Effective elastic thicknessAnatolian plateauTurkey doublet earthquakesBayesian optimization
《大地测量与地球动力学(英文版)》 2024 (003)
209-218 / 10
This research is funded by the National Natural Science Foun-dation of China(Grant Nos.U1939205,41974095)and the Basic Research Fund of the Institute of Geophysics,China Earthquake Administration(Grant Nos.DQJB21R30).We would like to thank the editors and three anonymous reviewers for their constructive comments,which helped improve the paper considerably.This work used the open-source software Geoist[65](https://cea2020.gitee.io/geoistdoc).
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