Abstract
A devastating doublet of earthquakes with moment magnitude MW 7.9 and MW 7.6 earthquakes contiguously occurred in SE Türkiye near the NW border of Syria. Here we perform a potency-density tensor inversion to simultaneously estimate rupture evolution and fault geometry for the doublet. We find the initial MW 7.9 earthquake involved discrete episodes of supershear rupture and back-rupture propagation, and was triggered by initial rupture along a bifurcated splay of the East Anatolian Fault. The second MW 7.6 event was triggered by the earlier MW 7.9 event, and it involved more extensive supershear rupture along a favorably curved fault, and was likely stopped by geometric barriers at the fault ends. Our results highlight the multi-scale cascading rupture growth across the complex fault network that affects the diverse rupture geometries of the 2023 Türkiye earthquake doublet, contributing to the strong ground shaking and associated devastation.
Original language | English |
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Article number | e2023GL103480 |
Journal | Geophysical Research Letters |
Volume | 50 |
Issue number | 12 |
DOIs | |
Publication status | Published - 28 Jun 2023 |
Bibliographical note
Publisher Copyright:© 2023. The Authors.
Funding
We thank the editor Germán Prieto and the reviewer Erdinc Saygin and the anonymous reviewer for their thorough evaluations and providing constructive comments and suggestions. We also thank Ahmed Ettaf Elbanna, František Gallovič, and Jiří Zahradník for fruitful discussion. The facilities of IRIS Data Services, and specifically the IRIS Data Management Center, were used for access to waveforms, related metadata, and/or derived products used in this study. IRIS Data Services are funded through the Seismological Facilities for the Advancement of Geoscience (SAGE) Award of the National Science Foundation under Cooperative Support Agreement EAR‐1851048. We appreciate the Disaster and Emergency Management Presidency of Türkiye (AFAD) for providing an initial catalogue of aftershocks and phase‐arrival data acquired from their bulletin resources. This work was supported by JSPS Grant‐in‐Aid for Scientific Research (C) 19K04030 and 22K03751, JSPS Early‐Career Scientists 20K14570, and JSPS Grant‐in‐Aid for Special Purposes 22K21372. The authors declare no conflicts of interest relevant to this study.
Funders | Funder number |
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National Science Foundation | EAR‐1851048 |
Japan Society for the Promotion of Science | 22K21372, 20K14570, 19K04030, 22K03751 |
Keywords
- complex fault geometry
- earthquake
- inversion
- rupture process
- teleseismic waves
- triggering