Manifestation features of near-surface sedimentary rock electric and acoustic responses on seismic waves from earthquakes

Muratov, Pavel; Rulenko, O. P.; Marapulets, Yu. V.

doi:10.1051/e3sconf/201912702015

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Cited by 3 publications

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Seismoacoustic and Seismoelectric Responses of Near-Surface Sedimentary Rocks in Kamchatka

Mishchenko,

Rulenko,

Marapulets

2023

Springer Proceedings in Earth and Environmental Sciences

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Seismoacoustic and Seismoelectric Responses of Near-Surface Sedimentary Rocks in Kamchatka

Mishchenko,

Rulenko,

Marapulets

2023

Springer Proceedings in Earth and Environmental Sciences

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Some features of acoustic and electric responses of near-surface sedimentary rocks during deformations by seismic waves from strong earthquakes (M_w > 6.5)

2020

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Acoustic and electric responses of near-surface sedimentary rocks are considered. They were recorded during the deformations by seismic waves from six earthquakes with magnitude Mw = 6.6-7.7 at the distances of 131-728 km from epicenters in Kamchatka region. Behavior of both responses during soil displacement and displacement velocity during wave propagation are un-der the analysis. The dependence of intensity and character of the responses manifestation on earthquake magnitude and the distance to its source had been discovered by the authors earlier and is confirmed in the work. It was discov-ered that the occurrence of acoustic response in kilohertz range correlates well with the behavior of soil displacement velocity vector and its spectrum.

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Analysis of manifestation of joint acoustic and electric responses of near-surface sedimentary rocks on the deformation by earthquake seismic waves in the South of Kamchatka

2021

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We continue the investigation of earlier discovered joint acoustic and electric responses of near-surface sedimentary rocks on the deformation by earthquake seismic waves. The appearance and absence of this response in earthquakes with the energy class of more than 11.0, which occurred from June 2017 to May 2021 by the eastern coast of Kamchatka in the latitude band of 51.7-54.0° N, are under consideration. From those earthquakes we selected 52 events, the seismic waves of which had rock acoustic response at Karymshina site, IKIR FEB RAS. Occurrences of joint acoustic and electric responses of rocks and manifestations of their low-frequency and high-frequency acoustic responses were analyzed. Applying the nonparametric correlation Spearman analysis, statistically significant relation between the energy class of the earthquakes under consideration and the distance from hypocenter to the observation site was discovered.

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Manifestation features of near-surface sedimentary rock electric and acoustic responses on seismic waves from earthquakes

Cited by 3 publications

References 4 publications

Seismoacoustic and Seismoelectric Responses of Near-Surface Sedimentary Rocks in Kamchatka

Seismoacoustic and Seismoelectric Responses of Near-Surface Sedimentary Rocks in Kamchatka

Some features of acoustic and electric responses of near-surface sedimentary rocks during deformations by seismic waves from strong earthquakes (M_w > 6.5)

Analysis of manifestation of joint acoustic and electric responses of near-surface sedimentary rocks on the deformation by earthquake seismic waves in the South of Kamchatka

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Manifestation features of near-surface sedimentary rock electric and acoustic responses on seismic waves from earthquakes

Cited by 3 publications

References 4 publications

Seismoacoustic and Seismoelectric Responses of Near-Surface Sedimentary Rocks in Kamchatka

Seismoacoustic and Seismoelectric Responses of Near-Surface Sedimentary Rocks in Kamchatka

Some features of acoustic and electric responses of near-surface sedimentary rocks during deformations by seismic waves from strong earthquakes (Mw > 6.5)

Analysis of manifestation of joint acoustic and electric responses of near-surface sedimentary rocks on the deformation by earthquake seismic waves in the South of Kamchatka

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Resources

About

Some features of acoustic and electric responses of near-surface sedimentary rocks during deformations by seismic waves from strong earthquakes (M_w > 6.5)