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Volume 31 Issue 5
Oct 2020
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Anatoly Kuzmich Rybin, Elena Anatol'evna Bataleva, SeKseniia Nepeina Nepeina, Pavel Alexandrovich Kaznacheev, Pavel Alexandrovich Matiukov, Pavel Nikolaevich Aleksandrov. 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. Journal of Earth Science, 2020, 31(5): 988-992. doi: 10.1007/s12583-020-1327-5
Citation: Anatoly Kuzmich Rybin, Elena Anatol'evna Bataleva, SeKseniia Nepeina Nepeina, Pavel Alexandrovich Kaznacheev, Pavel Alexandrovich Matiukov, Pavel Nikolaevich Aleksandrov. 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. Journal of Earth Science, 2020, 31(5): 988-992. doi: 10.1007/s12583-020-1327-5

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

doi: 10.1007/s12583-020-1327-5
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  • Corresponding author: Kseniia Sergeevna Nepeina, ORCID: 0000-0003-0725-8023, nepeina.k@mail.ru
  • Received Date: 24 May 2019
  • Accepted Date: 09 Apr 2020
  • Publish Date: 20 Oct 2020
  • 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.

     

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