Xiaotian Xue , Shunping Pei , Zhi Wang , Hanlin Liu , Wei Liu , Lei Li , Jiawei Li , Qian Hua
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引用次数: 0
Abstract
On February 6, 2023, the Türkiye Earthquake Doublet, consisting of two major earthquakes with magnitudes of MW7.8 and MW7.5, respectively, occurred within 9 h and devastated the Kahramanmaraş province in southwest Turkey. The geodynamic background of this area is exceedingly complicated owing to the combined action of the Anatolian Plate and the neighboring Eurasian, African, and Arabian plates, which contain many faults, the most prominent of which is the East Anatolian Fault Zone (EAFZ). These two earthquakes occurred on the Pazarcık Segment (PAZ.S) of the EAFZ and the Çardak Fault (CAR. F). The investigation of co-seismic changes in the velocity structure of the subterranean medium inside the focus area is critical for our understanding of earthquake ruptures. We chose <styled-content style-type="number">51572</styled-content> travel times before the earthquake doublet from January 1, 2014, to February 5, 2023, and <styled-content style-type="number">88371</styled-content> travel times after the earthquakes from February 6 to March 5, 2023, and utilized time-lapse tomography to derive the co-seismic changes in P-wave velocity. The results demonstrated that the P-wave velocity decreased around the center zone, with considerable surface displacement from the two earthquakes caused by rock breakup and stress release. The P-wave velocity increased in two areas: east of the Pazarcik Earthquake, where the Bozova Fault is located, and west of the Elbistan Earthquake. We believe that these two locations are compression zones generated by the strike-slip surface displacement. Similarly, the decrease in velocity in the areas adjacent to the Malatya Fault (MAL.F) and between the Amanos Segment (AM.S) of the EAFZ and the Savur Fault (SA.F) shows that these two locations were exposed to tension as a result of the co-seismic horizontal displacement on the surface. This study showed that in addition to the area close to the epicenter, the large earthquake can affect the velocity structure of faults far away from the main shock.
期刊介绍:
Earthquake Science (EQS) aims to publish high-quality, original, peer-reviewed articles on earthquake-related research subjects. It is an English international journal sponsored by the Seismological Society of China and the Institute of Geophysics, China Earthquake Administration.
The topics include, but not limited to, the following
● Seismic sources of all kinds.
● Earth structure at all scales.
● Seismotectonics.
● New methods and theoretical seismology.
● Strong ground motion.
● Seismic phenomena of all kinds.
● Seismic hazards, earthquake forecasting and prediction.
● Seismic instrumentation.
● Significant recent or past seismic events.
● Documentation of recent seismic events or important observations.
● Descriptions of field deployments, new methods, and available software tools.
The types of manuscripts include the following. There is no length requirement, except for the Short Notes.
【Articles】 Original contributions that have not been published elsewhere.
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【Review Articles】Review articles are by invitation only. Please contact the editorial office and editors for possible proposals.
【Toolboxes】 Descriptions of novel numerical methods and associated computer codes.
【Data Products】 Documentation of datasets of various kinds that are interested to the community and available for open access (field data, processed data, synthetic data, or models).
【Opinions】Views on important topics and future directions in earthquake science.
【Comments and Replies】Commentaries on a recently published EQS paper is welcome. The authors of the paper commented will be invited to reply. Both the Comment and the Reply are subject to peer review.