2023
DOI: 10.1785/0320230007
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The Destructive Earthquake Doublet of 6 February 2023 in South-Central Türkiye and Northwestern Syria: Initial Observations and Analyses

Abstract: On 6 February 2023, two large earthquakes with magnitude 7.8 and 7.6 rocked south-central Türkiye and northwestern Syria. At the time of writing, the death toll exceeded 50,000 in Türkiye and 7200 in Syria. The epicenter of the first mainshock was located ∼15 km east of the east Anatolian fault (EAF), the second large earthquake (9 hr later) initiated ∼90 km to the north on the east–west-trending Sürgü fault. Aftershocks delineate fault lengths of ∼350 and ∼170 km, respectively. Using satellite and seismic dat… Show more

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Cited by 80 publications
(31 citation statements)
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“…At large scales, earthquake gates can cause complex long‐term event histories with the behavior determined by stress conditions and other physical conditions (e.g., Rodriguez Padilla et al., 2022). Rupture complexities are manifest as complex source time functions (e.g., Yin et al., 2021) or as speedups and slowdowns in rupture velocity, that might be detectable with back‐projection imaging (e.g., Mai et al., 2023; Meng et al., 2011). Our experiments show that this can also happen at a smaller scale: distinct rupture phases initiate and terminate as mediated by the bump.…”
Section: Discussionmentioning
confidence: 99%
“…At large scales, earthquake gates can cause complex long‐term event histories with the behavior determined by stress conditions and other physical conditions (e.g., Rodriguez Padilla et al., 2022). Rupture complexities are manifest as complex source time functions (e.g., Yin et al., 2021) or as speedups and slowdowns in rupture velocity, that might be detectable with back‐projection imaging (e.g., Mai et al., 2023; Meng et al., 2011). Our experiments show that this can also happen at a smaller scale: distinct rupture phases initiate and terminate as mediated by the bump.…”
Section: Discussionmentioning
confidence: 99%
“…Although our sole use of teleseismic data may not rigorously discriminate the absolute location of the slip on the closely located parallel faults, we favor that the apparent back-propagating part of the rupture occurred on the main EAF because of the higher potency rate on the main EAF model fault rather than on the splay model fault (Figures 2c and 2d). This assumption is supported by independent modeling using geodetic datasets that finds larger slip along the main EAF than on the splay fault (Barbot et al, 2023;Mai et al, 2023;Melgar et al, 2023).…”
Section: Rupture Dynamics During Apparent Back-propagating Slipmentioning
confidence: 91%
“…The red line is the simulation result, and the black line is the data provided by Mai et al. (2023). The two blue dashed lines represent the intersections of Nurdağı‐Pazarcık Fault (left) and F3 (right) with East Anatolian Fault, respectively.…”
Section: Resultsmentioning
confidence: 99%
“…The detailed investigation results of surface rupture have not been seen yet, hence the surface strike‐slip is compared with the on‐fault displacement measured by Mai et al. (2023) based on the satellite data (Liu, Hu, Li, Ma, Shi, et al., 2022; Liu, Hu, Li, Ma, Wu, et al., 2022; Figure 3e). We have captured the first‐order characteristics of surface displacement.…”
Section: Resultsmentioning
confidence: 99%
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