地形学和构造物理方法在西北高加索和沃罗涅日板块地震活动性分析中的新可能性

IF 0.3 Q4 GEOCHEMISTRY & GEOPHYSICS Seismic Instruments Pub Date : 2022-05-23 DOI:10.3103/S0747923922030021
A. O. Agibalov, V. A. Zaitsev, A. A. Sentsov
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引用次数: 0

摘要

本文展示了对地形进行复杂形态分析和现代地球动力学计算机模拟的可能性,以确定在地震构造方面得到充分研究的两个不同地区的地震活动性区域:西北高加索和沃罗涅日前陆。在定量层面上,大多数地震震中与地形的一些形态特征(垂直解剖的深度、斜坡的陡度、轮廓和延伸线的密度等)值增加的区域有关。计算机模拟已被用于确定可能形成新裂缝的区域,其中分别有80%和65%的地震震中位于高加索西北部和沃罗涅日前断层。这些地区的面积份额分别为55%(高加索西北部)和36%(沃罗涅日前),这表明所获得的结果具有信息性。这项研究意义重大,因为在尚未进行详细地震观测的地区划定推断地震活跃区时,可能需要使用这些方法和方法。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

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New Possibilities of Geomorphological and Tectonophysical Methods for Analyzing Seismicity as Applied to the Northwestern Caucasus and Voronezh Anteclise

The paper shows the possibilities of complex morphometric analysis of the relief and computer modeling of modern geodynamics to identify seismically active areas in two different regions well studied in seismotectonic terms: the Northwestern Caucasus and the Voronezh anteclise. At the quantitative level, the majority of earthquake epicenters are associated with areas of increased values of a number of morphometric characteristics of the relief (depth of vertical dissection, steepness of slopes, density of lineaments and elongation lines, etc.). Computer modeling has been used to identify areas of possible formation of new fractures, within which 80 and 65% of earthquake epicenters of the Northwestern Caucasus and Voronezh anteclise, respectively, are located. The shares of the area of these regions are 55% (for the Northwestern Caucasus) and 36% (for the Voronezh anteclise), which indicates the informative nature of the results obtained. The research is significant, because the methods and approaches used may be in demand when delineating inferred seismically active areas of territories where detailed seismological observations have not been carried out.

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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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