Abstract
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.
Similar content being viewed by others
Change history
27 December 2020
The original version of this article unfortunately contained a mistake. The presentation of an author’s name was incorrect. The corrected one is given below.
References Cited
Aleksandrov, P. N., 2009. The Theory of Seismic and Electromagnetic Monitoring of the Modern Geodynamic Processes. Bulletin of Kamchatka Regional Association: Earth Sciences, 2(14): 49–58 (in Russian with English Abstract)
Bataleva, E. A., Przhiyalgovskii, E. S., Batalev, V. Y., et al., 2017. New Data on the Deep Structure of the South Kochkor Zone of Concentrated Deformation. Doklady Earth Sciences, 475(2): 930–934. https://doi.org/10.1134/s1028334x1708013x
Buslov, M. M., De Grave, J., Bataleva, E. A. V., et al., 2007. Cenozoic Tectonic and Geodynamic Evolution of the Kyrgyz Tien Shan Mountains: A Review of Geological, Thermochronological and Geophysical Data. Journal of Asian Earth Sciences, 29(2/3): 205–214. https://doi.org/10.1016/j.jseaes.2006.07.001
Karplus, M., Schmandt, B., 2018. Preface to the Focus Section on Geophone Array Seismology. Seismological Research Letters, 89(5): 1597–1600. https://doi.org/10.1785/0220180212
Kaznacheev, P. A., Matiukov, V. E., Aleksandrov, P. N., et al., 2019. Development of a Three-Axis Gradient System for Seismoacoustic Data Acquisition in Geodynamically Active Regions. Seismic Instruments, 55(5): 535–543. https://doi.org/10.3103/s0747923919050062
Khavroshkin, O. B., 1999. Some Problems of Nonlinear Seismology. OIFZ RAS, 286 (in Russian)
Korn, G. A., Korn, T. M., 1968. Mathematical Handbook: For Scientists and Engineers. McGraw-Hill Book Company, New York
Langston, C. A., 2007. Wave Gradiometry in the Time Domain. Bulletin of the Seismological Society of America, 97(3): 926–933. https://doi.org/10.1785/0120060152
Lin, F. C., Li, D., Clayton, R. W., et al., 2013. High-Resolution 3D Shallow Crustal Structure in Long Beach, California: Application of Ambient Noise Tomography on a Dense Seismic Array. Geophysics, 78: 45–56. https://doi.org/10.1190/geo2012-0453.1
Maeda, T., Nishida, K., Takagi, R., et al., 2016. Reconstruction of a 2D Seismic Wavefield by Seismic Gradiometry. Progress in Earth and Planetary Science, 3(1): 31. https://doi.org/10.1186/s40645-016-0107-4
Moura, R. M., Senos Matias, M. J., 2012. Geophones on Blocks: A Prototype Towable Geophone System for Shallow Land Seismic Investigations. Geophysical Prospecting, 60(1): 192–200. https://doi.org/10.1111/j.1365-2478.2011.00963.x
Picozzi, M., Parolai, S., Bindi, D., et al., 2009. Characterization of Shallow Geology by High-Frequency Seismic Noise Tomography. Geophysical Journal International, 176(1): 164–174. https://doi.org/10.1111/j.1365-246x.2008.03966.x
Schmelzbach, C., Donner, S., Igel, H., et al., 2018. Advances in 6C Seismology: Applications of Combined Translational and Rotational Motion Measurements in Global and Exploration Seismology. Geophysics, 83(3): WC53–WC69. https://doi.org/10.1190/geo2017-0492.1
Sobolev, G. A., Ponomarev, A. V., Kol’tsov, A. V., et al., 2001. Excitation of Acoustic Emission by Elastic Impulses. Izvestiya-Physics of the Solid Earth, 37(1): 73–77
Acknowledgments
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). We are also thankful to the reviewers for their comments and the Editor-in-Chief and all editors of the Journal of Earth Science enabling our research to be published. The final publication is available at Springer via https://doi.org/10.1007/s12583-020-1327-5.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Rybin, A.K., Bataleva, E.A., Nepeina, K.S. et al. 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. J. Earth Sci. 31, 988–992 (2020). https://doi.org/10.1007/s12583-020-1327-5
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s12583-020-1327-5