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Super-shear ruptures steered by pre-stress heterogeneities during the 2023 Kahramanmaraş earthquake doublet

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Abstract

The 2023 M7.8 and M7.5 earthquake doublet near Kahramanmaraş, Turkey, provides insight regarding how large earthquakes rupture complex faults. Here we determine the faults geometry using surface ruptures and Synthetic Aperture Radar measurements, and the rupture kinematics from the joint inversion of high-rate Global Navigation Satellite System (GNSS), strong-motion waveforms, and GNSS static displacement. The M7.8 event initiated on a splay fault and subsequently propagated along the main East Anatolian Fault with an average rupture velocity between 3.0 and 4.0 km/s. In contrast, the M7.5 event demonstrated a bilateral supershear rupture of about 5.0–6.0 km/s over an 80 km length. Despite varying strike and dip angles, the sub-faults involved in the mainshock are nearly optimally oriented relative to the local stress tensor. The second event ruptured a fault misaligned with respect to the regional stress, also hinting at the effect of local stress heterogeneity in addition to a possible free surface effect.
Original languageEnglish
Article number7004
Pages (from-to)1-11
Number of pages11
JournalNature Communications
Volume15
Issue number1
DOIs
Publication statusPublished (in print/issue) - 14 Aug 2024

Bibliographical note

Publisher Copyright:
© The Author(s) 2024.

Data Availability Statement

GNSS data used in this study were obtained from the Turkish Permanent GNSS Network (TUSAGA-Aktif) and are available at https://www.
tusaga-aktif.gov.tr/Web/DepremVerileri.aspx. Strong motion records
were provided by AFAD (https://tdvms.afad.gov.tr/list-station/543428/
37.043/37.288, https://tdvms.afad.gov.tr/list-station/543593/37.239/
38.089). ALOS-2 data are made freely available by the Japan Aerospace Exploration Agency (JAXA) at: https://www.eorc.jaxa.jp/ALOS/
en/dataset/alos_open_and_free_e.htm. Sentinel-1 data are also freely
available and provided by the European Space Agency (ESA) under the Copernicus Program.

Funding

K.C. was funded by the National Natural Science Foundation of China (NSFC) 42074024 and Guangdong Provincial Key Laboratory of Geophysical High-resolution Imaging Technology (2022B1212010002). C.M. was supported by the NASA Earth Surface and Interior Focus Area ROSES grants (80NM0018D0004, 80NSSC20K0492). L.D.Z was supported by the European Research Council (ERC) Synergy Grant “Fault Activation and Earthquake Rupture” (FEAR) (No. 856559), the Earth Observatory of Singapore (EOS), and the Singapore Ministry of Education Tier 3b project “Investigating Volcano and Earthquake Science and Technology (InVEST)” (Award No. MOE-MOET32021-0002). C.L. was supported by NSFC 42274026 and J.P.A was supported by NASA/ROSES grant 80NSSC20K0492. We thank JAXA for providing ALOS-2 data used in this study.

FundersFunder number
European Research Council
2022B1212010002
National Aeronautics and Space Administration80NSSC20K0492, 80NM0018D0004
National Natural Science Foundation of China42074024
856559
42274026, MOE-MOET32021-0002

    UN SDGs

    This output contributes to the following UN Sustainable Development Goals (SDGs)

    1. SDG 15 - Life on Land
      SDG 15 Life on Land

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