Standard

About usage of weak anisotropy model in dowhole microseismic monitoring applications. / Yaskevich, S. V.; Duchkov, A. A.; Plotnitskiy, P. S. и др.

Horizontal Wells 2017. European Association of Geoscientists and Engineers, EAGE, 2017.

Результаты исследований: Публикации в книгах, отчётах, сборниках, трудах конференций › статья в сборнике материалов конференции › научная › Рецензирование

Harvard

Yaskevich, SV, Duchkov, AA, Plotnitskiy, PS & Myasnikov, AV 2017, About usage of weak anisotropy model in dowhole microseismic monitoring applications. в Horizontal Wells 2017. European Association of Geoscientists and Engineers, EAGE, Horizontal Wells 2017: Challenges and Opportunities, Kazan, Российская Федерация, 15.05.2017. https://doi.org/10.3997/2214-4609.201700465

APA

Yaskevich, S. V., Duchkov, A. A., Plotnitskiy, P. S., & Myasnikov, A. V. (2017). About usage of weak anisotropy model in dowhole microseismic monitoring applications. в Horizontal Wells 2017 European Association of Geoscientists and Engineers, EAGE. https://doi.org/10.3997/2214-4609.201700465

Vancouver

Yaskevich SV, Duchkov AA, Plotnitskiy PS, Myasnikov AV. About usage of weak anisotropy model in dowhole microseismic monitoring applications. в Horizontal Wells 2017. European Association of Geoscientists and Engineers, EAGE. 2017 doi: 10.3997/2214-4609.201700465

Author

Yaskevich, S. V. ; Duchkov, A. A. ; Plotnitskiy, P. S. и др. / About usage of weak anisotropy model in dowhole microseismic monitoring applications. Horizontal Wells 2017. European Association of Geoscientists and Engineers, EAGE, 2017.

BibTeX

@inproceedings{265bde3d9db44db6b80acdc811ae2623,
title = "About usage of weak anisotropy model in dowhole microseismic monitoring applications",
abstract = "For downhole microseismic monitoring velocity model building, is a necessary step in the processing of data and is considered one of the main factors controlling the accuracy of the hypocenter location. In this paper we analyzed the possibility of using the weak anisotropy approximation to locate microseismic events hypocenters. The use of weak anisotropy model reduces the computational cost, and it was shown that for some cases it works well.",
author = "Yaskevich, {S. V.} and Duchkov, {A. A.} and Plotnitskiy, {P. S.} and Myasnikov, {A. V.}",
year = "2017",
doi = "10.3997/2214-4609.201700465",
language = "English",
booktitle = "Horizontal Wells 2017",
publisher = "European Association of Geoscientists and Engineers, EAGE",
note = "Horizontal Wells 2017: Challenges and Opportunities ; Conference date: 15-05-2017 Through 19-05-2017",

}

RIS

TY - GEN

T1 - About usage of weak anisotropy model in dowhole microseismic monitoring applications

AU - Yaskevich, S. V.

AU - Duchkov, A. A.

AU - Plotnitskiy, P. S.

AU - Myasnikov, A. V.

PY - 2017

Y1 - 2017

N2 - For downhole microseismic monitoring velocity model building, is a necessary step in the processing of data and is considered one of the main factors controlling the accuracy of the hypocenter location. In this paper we analyzed the possibility of using the weak anisotropy approximation to locate microseismic events hypocenters. The use of weak anisotropy model reduces the computational cost, and it was shown that for some cases it works well.

AB - For downhole microseismic monitoring velocity model building, is a necessary step in the processing of data and is considered one of the main factors controlling the accuracy of the hypocenter location. In this paper we analyzed the possibility of using the weak anisotropy approximation to locate microseismic events hypocenters. The use of weak anisotropy model reduces the computational cost, and it was shown that for some cases it works well.

UR - http://www.scopus.com/inward/record.url?scp=85027189772&partnerID=8YFLogxK

U2 - 10.3997/2214-4609.201700465

DO - 10.3997/2214-4609.201700465

M3 - Conference contribution

AN - SCOPUS:85027189772

BT - Horizontal Wells 2017

PB - European Association of Geoscientists and Engineers, EAGE

T2 - Horizontal Wells 2017: Challenges and Opportunities

Y2 - 15 May 2017 through 19 May 2017

ER -

ID: 9033353