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Abstract
Two major earthquakes (Mw 7.8 and Mw 7.7) struck southeastern Türkiye on February 6, 2023, causing significant damage. Kinematic rupture models, derived from seismic and geodetic data using complex fault models, reveal that the larger event propagated bilaterally along the East Anatolian Fault Zone (EAFZ). The second event, 9 hours later, ruptured along a curved northern EAFZ strand. Coulomb Failure stress increase from the first event plausibly triggered the second.
Publisher
Nature Communications
Published On
Sep 09, 2023
Authors
Chengli Liu, Thorne Lay, Rongjiang Wang, Tuncay Taymaz, Zujun Xie, Xiong Xiong, Tahir Serkan Irmak, Metin Kahraman, Ceyhun Erman
Tags
earthquake
East Anatolian Fault Zone
kinematic rupture models
Coulomb Failure stress
Türkiye
seismic data
geodetic data
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