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Acoustic method for defining the stress state of a rock massif based on solution of the seismic inverse problem. / Nazarov, L. A.; Nazarova, L. A.; Romenskii, E. I. et al.

In: Doklady Earth Sciences, Vol. 466, No. 2, 01.02.2016, p. 210-213.

Research output: Contribution to journal › Article › peer-review

Harvard

Nazarov, LA, Nazarova, LA, Romenskii, EI, Tcheverda, VA & Epov, MI 2016, 'Acoustic method for defining the stress state of a rock massif based on solution of the seismic inverse problem', Doklady Earth Sciences, vol. 466, no. 2, pp. 210-213. https://doi.org/10.1134/S1028334X16020215

APA

Nazarov, L. A., Nazarova, L. A., Romenskii, E. I., Tcheverda, V. A., & Epov, M. I. (2016). Acoustic method for defining the stress state of a rock massif based on solution of the seismic inverse problem. Doklady Earth Sciences, 466(2), 210-213. https://doi.org/10.1134/S1028334X16020215

Vancouver

Nazarov LA, Nazarova LA, Romenskii EI, Tcheverda VA, Epov MI. Acoustic method for defining the stress state of a rock massif based on solution of the seismic inverse problem. Doklady Earth Sciences. 2016 Feb 1;466(2):210-213. doi: 10.1134/S1028334X16020215

Author

Nazarov, L. A. ; Nazarova, L. A. ; Romenskii, E. I. et al. / Acoustic method for defining the stress state of a rock massif based on solution of the seismic inverse problem. In: Doklady Earth Sciences. 2016 ; Vol. 466, No. 2. pp. 210-213.

BibTeX

@article{7de7d37e7b8945d3b49b3bf3ec28f66b,
title = "Acoustic method for defining the stress state of a rock massif based on solution of the seismic inverse problem",
abstract = "A method for estimating the stress–strain state of a rock massif in the vicinity of underground facilities is substantiated. This method is based on solution of the boundary inverse problem of defining the components of an external stress field from the acoustic sounding data. The acoustic sounding data used are the arrival times of diving head longitudinal waves, recorded in a long mine shaft. Numerical experiments have revealed the optimal arrangement of the recording network and the limited relative error in the input data, which, taken together, provide for solvability of the inverse problem.",
author = "Nazarov, {L. A.} and Nazarova, {L. A.} and Romenskii, {E. I.} and Tcheverda, {V. A.} and Epov, {M. I.}",
year = "2016",
month = feb,
day = "1",
doi = "10.1134/S1028334X16020215",
language = "English",
volume = "466",
pages = "210--213",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - Acoustic method for defining the stress state of a rock massif based on solution of the seismic inverse problem

AU - Nazarov, L. A.

AU - Nazarova, L. A.

AU - Romenskii, E. I.

AU - Tcheverda, V. A.

AU - Epov, M. I.

PY - 2016/2/1

Y1 - 2016/2/1

N2 - A method for estimating the stress–strain state of a rock massif in the vicinity of underground facilities is substantiated. This method is based on solution of the boundary inverse problem of defining the components of an external stress field from the acoustic sounding data. The acoustic sounding data used are the arrival times of diving head longitudinal waves, recorded in a long mine shaft. Numerical experiments have revealed the optimal arrangement of the recording network and the limited relative error in the input data, which, taken together, provide for solvability of the inverse problem.

AB - A method for estimating the stress–strain state of a rock massif in the vicinity of underground facilities is substantiated. This method is based on solution of the boundary inverse problem of defining the components of an external stress field from the acoustic sounding data. The acoustic sounding data used are the arrival times of diving head longitudinal waves, recorded in a long mine shaft. Numerical experiments have revealed the optimal arrangement of the recording network and the limited relative error in the input data, which, taken together, provide for solvability of the inverse problem.

UR - http://www.scopus.com/inward/record.url?scp=84962730065&partnerID=8YFLogxK

U2 - 10.1134/S1028334X16020215

DO - 10.1134/S1028334X16020215

M3 - Article

AN - SCOPUS:84962730065

VL - 466

SP - 210

EP - 213

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 25777245