The article considers the problem of microseismic sounding with microseisms excited by deep earthquake foci. A model of a plane seismic wave is constructed, crossing a layered structure from the Earth’s interior. In this case, the distribution of elastic parameters in the Earth’s crust can be determined by measuring the displacement field on the surface.
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E. V. Rabinovich, A. S. Turkin, and Yu. L. Novakovskii, “Above-ground location of microseismic signals for monitoring a hydraulic discontinuity of a layer,” Dokl. TUSUR, No. 1(25), part 1, 104–112 (2012).
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Translated from Prikladnaya Matematika i Informatika, No. 45, 2014, pp. 41–46.
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Dmitriev, V.I., Yan, CS. A Mathematical Model of Microseismic Sounding. Comput Math Model 26, 163–167 (2015). https://doi.org/10.1007/s10598-015-9264-3
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DOI: https://doi.org/10.1007/s10598-015-9264-3