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Definition of the Seismic Field of the Underground Sources in the Ambient Seismic Noise in the Tien Shan Region Using a Three-Component Gradient System 被引量:2

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摘要 This paper considers a new approach to solving the problem of quantitative estimation of the microseism energy for underground sources that is based on the synthesis of noise interferometry and the passive seismic method of the gradient system. The selection of a seismic field of the underground sources is considered in an experiment conducted in the Tien Shan region. The peculiarities of approach include the separation of vertical microseisms in the ambient seismic noise field structure according to the data of the seismic gradient system and a passive noise interferometry diagram, where microseisms from the underground sources are used as the seismic signal source. It is shown that the use of noise interferometry and passive seismic gradient system allows using the synchronous microseism recordings in a small number of points for passive medium sensing, and leads to the restoration of unknown energy parameters of the seismic field of underground sources.
出处 《Journal of Earth Science》 SCIE CAS CSCD 2020年第5期988-992,共5页 地球科学学刊(英文版)
基金 The data processing programs,development and implementation of the gradient array system are partially performed with the grant support from the Russian Foundation for Basic Research(No.20-05-00475) The subjects relating to the correlation of geophysical parameters with the average stress-strain behaviour of the geological environment are explored within the Russian State Governmental Task of the Research Station of the Russian Academy of Sciences(No.AAAA-A19-119020190063-2)。
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