Identifying the Occurrence Time of the Destructive Kahramanmaras-Gazientep Earthquake of Magnitude M7.8 in Turkey on 6 February 2023

被引:0
|
作者
Sarlis, Nicholas V. [1 ,2 ]
Skordas, Efthimios S. [1 ,2 ]
Christopoulos, Stavros-Richard G. [2 ,3 ,4 ]
Varotsos, Panayiotis K. [5 ]
机构
[1] Natl & Kapodistrian Univ Athens, Sect Condensed Matter Phys, Dept Phys, Panepistimiopolis,Zografos, Athens 15784, Greece
[2] Natl & Kapodistrian Univ Athens, Solid Earth Phys Inst, Dept Phys, Panepistimiopolis,Zografos, Athens 15784, Greece
[3] Univ Huddersfield, Sch Comp & Engn, Dept Comp Sci, Huddersfield HD1 3DH, England
[4] Coventry Univ, Ctr Computat Sci & Math Modelling, Coventry CV1 2TU, England
[5] Hellen Fire Brigade, Dept Operat Informat & Geospatial Anal, Div Informat & Telecommun, Athens 18346, Greece
来源
APPLIED SCIENCES-BASEL | 2024年 / 14卷 / 03期
关键词
earthquakes; natural time; time-series; entropy; criticality; complex systems; DETRENDED FLUCTUATION ANALYSIS; NATURAL TIME; NOWCASTING EARTHQUAKES; MAJOR EARTHQUAKES; LATEST ASPECTS; PACIFIC COAST; DNA; SEISMICITY; PREDICTION; FEATURES;
D O I
10.3390/app14031215
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
Here, we employ natural time analysis of seismicity together with non-extensive statistical mechanics aiming at shortening the occurrence time window of the Kahramanmaras-Gazientep M7.8 earthquake. The results obtained are in the positive direction pointing to the fact that after 3 February 2023 at 11:05:58 UTC, a strong earthquake was imminent. Natural time analysis also reveals a minimum fluctuation of the order parameter of seismicity almost three and a half months before the M7.8 earthquake, pointing to the initiation of seismic electrical activity. Moreover, before this earthquake occurrence, the detrended fluctuation analysis of the earthquake magnitude time-series reveals random behavior. Finally, when applying earthquake nowcasting, we find average earthquake potential score values which are compatible with those previously observed before strong (M >= 7.1) earthquakes. The results obtained may improve our understanding of the physics of crustal phenomena that lead to strong earthquakes.
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页数:19
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