About usage of weak anisotropy model in dowhole microseismic monitoring applications

S. V. Yaskevich; A. A. Duchkov; P. S. Plotnitskiy; A. V. Myasnikov

doi:10.3997/2214-4609.201700465

About usage of weak anisotropy model in dowhole microseismic monitoring applications

S. V. Yaskevich, A. A. Duchkov, P. S. Plotnitskiy, A. V. Myasnikov

Результат исследования: Публикации в книгах, отчётах, сборниках, трудах конференций › статья в сборнике материалов конференции › научная › рецензирование

Аннотация

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.

Язык оригинала	английский
Название основной публикации	Horizontal Wells 2017
Издатель	European Association of Geoscientists and Engineers, EAGE
DOI	https://doi.org/10.3997/2214-4609.201700465
Состояние	Опубликовано - 2017
Событие	Horizontal Wells 2017: Challenges and Opportunities - Kazan, Российская Федерация Продолжительность: 15 мая 2017 → 19 мая 2017

Конференция

Конференция	Horizontal Wells 2017: Challenges and Opportunities
Страна	Российская Федерация
Город	Kazan
Период	15.05.2017 → 19.05.2017

Доступ к документу

10.3997/2214-4609.201700465

Link to publication in Scopus

Fingerprint Подробные сведения о темах исследования «About usage of weak anisotropy model in dowhole microseismic monitoring applications». Вместе они формируют уникальный семантический отпечаток (fingerprint).

Цитировать

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

@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",

}

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

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

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

Результат исследования: Публикации в книгах, отчётах, сборниках, трудах конференций › статья в сборнике материалов конференции › научная › рецензирование

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PY - 2017

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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.

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