The Bystrinskii Earthquake in the Southern Baikal Region (Sep. 21, 2020, Mw=5.4): General Characteristics, Basic Parameters, and Deformation Signs of the Transition of the Focus to the Meta-Unstable State

被引:3
作者
Bornyakov, S. A. [1 ,2 ]
Dobrynina, A. A. [1 ,2 ,3 ]
Seminsky, K. Zh [1 ,2 ]
Sankov, V. A. [1 ,2 ]
Radziminovich, N. A. [1 ]
Salko, D., V [1 ]
Shagun, A. N. [1 ]
机构
[1] Russian Acad Sci, Inst Earths Crust, Siberian Branch, Irkutsk 664033, Russia
[2] Russian Acad Sci, Irkutsk Res Ctr, Siberian Branch, Irkutsk 664033, Russia
[3] Russian Acad Sci, Geol Inst, Siberian Branch, Ulan Ude 670047, Russia
基金
中国国家自然科学基金; 俄罗斯基础研究基金会;
关键词
Southern Baikal region; the Bystrinskii earthquake; foreshocks; aftershocks; focal mechanism; deformation monitoring; meta-instability; precursor; STICK-SLIP; RIFT;
D O I
10.1134/S1028334X21050044
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The results of studying the Bystrinskii earthquake of September 21, 2020, in the southern Baikal region are presented. Its geodynamic position, focal mechanism, and basic parameters are indicated. The deformation monitoring data showing six days of anomalous growth of rock deformations preceding the earthquake are provided. It is shown that the scenario of the deformation process before the earthquake is similar to the scenario of preparing dynamic slip during the experimental simulation of the intermittent "stick-slip" process. On the basis of similarity in the implementation of deformation processes in nature and in the model, it is stated that the deformation anomaly, which appeared just before the Bystrinskii earthquake, is a regular phenomenon and can be considered as its short-term precursor.
引用
收藏
页码:427 / 431
页数:5
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