Rupture Process of the February 2023 Mw 7.8 Earthquake Sequence in South-Central Türkiye and Northwestern Syria From Teleseismic P-Wave Data
On February 6, 2023, two destructive earthquakes of Mw 7.8 and 7.6 struck the south-central part of Türkiye. The first event (E1) started on an off-fault branch near the East Anatolian Fault (EAF) and the second one (E2) occurred on the east-west trending Sürgü fault ~9 hours later. We use back-projection (BP) and finite fault inversion (FFI) with teleseismic P-wave to image the rupture process of these two earthquakes. For the BP, we use Alaskan stations and only target high cross-correlation coefficients (>0.6). The FFI uses 18 and 17 seismic recordings for E1 and E2, respectively, ensuring good azimuth coverage. We define segmented rupture-plane geometries using fault traces derived from satellite radar image pixel offset tracking. We parameterize E1 with 4 fault segments, each with a uniform dip of 89o, whereas E2 comprises 3 segments dipping 78o to the north. All segments are discretized into 5 x 5 km2 subfaults, on which we solve for slip, rupture onset time, and rise time. In addition, we explore the model space using Bayesian inference to account for the non-uniqueness of the inversion solution.
Both the BP and FFI results indicate bilateral rupture propagation for both earthquakes. The BP results for E1 show that the rupture propagated to the northeast along a fault branch until it reached the EAF, then it continued along EAF to the northeast for up to ~55 s. The rupture to the southwest along the EAF, towards the Hatay province, appears to have been delayed and then terminated at ~80 s. For E2, we observe frequency-dependent BP results due to the directivity effect. The BP captures the rupture to the east and then northeast in a lower frequency range (0.1-0.5 Hz), while it images opposite rupture direction to the west in a higher frequency range (0.5-1 Hz). The FFI result of E1 shows at least three high-slip patches with the maximum slip of up to 8 m. The slip model of E2 shows high slip of above 8 m near the surface of the Sürgü fault, but less slip to the northeast and southwest. Overall, our modeled moment magnitudes of the two events are Mw 7.97 and Mw 7.77, respectively.
Session: February 2023 Mw 7.8 Earthquake Sequence in Turkey [Poster]
Type: Poster
Room: Ballroom
Date: 4/19/2023
Presentation Time: 08:00 AM (local time)
Presenting Author: Cahli Suhendi
Student Presenter: Yes
Additional Authors
Cahli Suhendi Presenting Author Corresponding Author cahli.suhendi@kaust.edu.sa King Abdullah University of Science and Technology |
Bo Li bo.li.3@kaust.edu.sa King Abdullah University of Science and Technology |
Xing Li xing.li.1@kaust.edu.sa King Abdullah University of Science and Technology |
Kadek Hendrawan Palgunadi kadek.palgunadi@kaust.edu.sa King Abdullah University of Science and Technology |
Jihong Liu jihong.liu@kaust.edu.sa King Abdullah University of Science and Technology |
Yann Klinger klinger@ipgp.fr Université de Paris Cité, Institut de Physique de Globe, CNRS |
Sigurjón Jónsson sigurjon.jonsson@kaust.edu.sa King Abdullah University of Science and Technology |
Paul Martin Mai martin.mai@kaust.edu.sa King Abdullah University of Science and Technology |
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Rupture Process of the February 2023 Mw 7.8 Earthquake Sequence in South-Central Türkiye and Northwestern Syria From Teleseismic P-Wave Data
Category
February 2023 Mw 7.8 Earthquake Sequence in Turkey
Description