Vertical and Horizontal Displacements Based on Observations at Talaya Station (Southwest Part of the Baikal Rift)

IF 0.3 Q4 GEOCHEMISTRY & GEOPHYSICS Seismic Instruments Pub Date : 2025-03-06 DOI:10.3103/S0747923924700026
V. Yu. Timofeev, A. V. Timofeev, D. G. Ardyukov, I. S. Sizikov, D. A. Nosov
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Abstract

Rates of modern movements are an important factor in the modern geodynamics of the Baikal Rift System. Reflection of strong earthquakes in the experimental values of displacements is discussed, as well as the question of modern vertical movements. According to absolute gravimetry and space geodesy measurements of vertical and horizontal movement rates at the Talaya seismic station (Baikal Rift) for 1992–2022, the displacement rates were determined as 1.7–1.9 mm/year SEE with respect to the point of Irkutsk (Siberian Platform). A set of methods was used to obtain the vertical movement rates for different epochs prior to, during, and after the Kultuk earthquake (2008, M = 6.3, 25 km to epicenter). Subsidence rates vary from 1.1 to 3.3 mm/yr. Possible signs of preparation of Baikal earthquakes have been identified

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基于Talaya站(贝加尔湖裂谷西南段)观测的垂直和水平位移
现代运动速率是贝加尔湖裂谷系现代地球动力学的一个重要因素。讨论了强震在位移实验值中的反映,以及现代垂直运动问题。根据1992-2022年Talaya地震台站(贝加尔湖裂谷)垂直和水平运动速率的绝对重力测量和空间大地测量,确定伊尔库茨克(西伯利亚地台)点的位移速率为1.7-1.9 mm/年。利用一套方法获得Kultuk地震(2008年,M = 6.3,距震中25 km)前、中、后不同时期的垂直运动速率。沉降速率从1.1到3.3毫米/年不等。贝加尔湖可能发生地震的迹象已经被确定
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来源期刊
Seismic Instruments
Seismic Instruments GEOCHEMISTRY & GEOPHYSICS-
自引率
44.40%
发文量
45
期刊介绍: Seismic Instruments is a journal devoted to the description of geophysical instruments used in seismic research. In addition to covering the actual instruments for registering seismic waves, substantial room is devoted to solving instrumental-methodological problems of geophysical monitoring, applying various methods that are used to search for earthquake precursors, to studying earthquake nucleation processes and to monitoring natural and technogenous processes. The description of the construction, working elements, and technical characteristics of the instruments, as well as some results of implementation of the instruments and interpretation of the results are given. Attention is paid to seismic monitoring data and earthquake catalog quality Analysis.
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