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Imaging microseismic events by diffraction stacking with moment tensor inversion. / Anikiev, D.; Stan k, F.; Valenta, J.; Eisner, L.

SEG Technical Program Expanded Abstracts 2013. Society of Exploration Geophysicists, 2013. p. 2013-2018.

Research output: Chapter in Book/Report/Conference proceedingConference contributionResearch

Harvard

Anikiev, D, Stan k, F, Valenta, J & Eisner, L 2013, Imaging microseismic events by diffraction stacking with moment tensor inversion. in SEG Technical Program Expanded Abstracts 2013. Society of Exploration Geophysicists, pp. 2013-2018. https://doi.org/10.1190/segam2013-0830.1

APA

Anikiev, D., Stan k, F., Valenta, J., & Eisner, L. (2013). Imaging microseismic events by diffraction stacking with moment tensor inversion. In SEG Technical Program Expanded Abstracts 2013 (pp. 2013-2018). Society of Exploration Geophysicists. https://doi.org/10.1190/segam2013-0830.1

Vancouver

Anikiev D, Stan k F, Valenta J, Eisner L. Imaging microseismic events by diffraction stacking with moment tensor inversion. In SEG Technical Program Expanded Abstracts 2013. Society of Exploration Geophysicists. 2013. p. 2013-2018 https://doi.org/10.1190/segam2013-0830.1

Author

Anikiev, D. ; Stan k, F. ; Valenta, J. ; Eisner, L. / Imaging microseismic events by diffraction stacking with moment tensor inversion. SEG Technical Program Expanded Abstracts 2013. Society of Exploration Geophysicists, 2013. pp. 2013-2018

BibTeX

@inproceedings{5b6a01e421614378930df315208fb678,
title = "Imaging microseismic events by diffraction stacking with moment tensor inversion",
abstract = "Microseismic monitoring can greatly benefit from imaging events with low signal-to-noise ratio as the number of low signal events grows exponentially. Hence, developing a migration-type detection and location technique has a potential to greatly improve microseismic monitoring. We developed a new methodology using stacking of seismic phases and amplitudes along diffraction traveltime curves together with polarization correction by seismic moment tensor inversion. This provided a calibrated model and imaged the perforation shots as non-shear events. We processed one day of data from microseismic monitoring of shale stimulation. The induced events are mostly shear events forming trends along the maximum horizontal stress direction and above the injection intervals.",
author = "D. Anikiev and {Stan k}, F. and J. Valenta and L. Eisner",
year = "2013",
doi = "10.1190/segam2013-0830.1",
language = "English",
pages = "2013--2018",
booktitle = "SEG Technical Program Expanded Abstracts 2013",
publisher = "Society of Exploration Geophysicists",
address = "United States",

}

RIS

TY - GEN

T1 - Imaging microseismic events by diffraction stacking with moment tensor inversion

AU - Anikiev, D.

AU - Stan k, F.

AU - Valenta, J.

AU - Eisner, L.

PY - 2013

Y1 - 2013

N2 - Microseismic monitoring can greatly benefit from imaging events with low signal-to-noise ratio as the number of low signal events grows exponentially. Hence, developing a migration-type detection and location technique has a potential to greatly improve microseismic monitoring. We developed a new methodology using stacking of seismic phases and amplitudes along diffraction traveltime curves together with polarization correction by seismic moment tensor inversion. This provided a calibrated model and imaged the perforation shots as non-shear events. We processed one day of data from microseismic monitoring of shale stimulation. The induced events are mostly shear events forming trends along the maximum horizontal stress direction and above the injection intervals.

AB - Microseismic monitoring can greatly benefit from imaging events with low signal-to-noise ratio as the number of low signal events grows exponentially. Hence, developing a migration-type detection and location technique has a potential to greatly improve microseismic monitoring. We developed a new methodology using stacking of seismic phases and amplitudes along diffraction traveltime curves together with polarization correction by seismic moment tensor inversion. This provided a calibrated model and imaged the perforation shots as non-shear events. We processed one day of data from microseismic monitoring of shale stimulation. The induced events are mostly shear events forming trends along the maximum horizontal stress direction and above the injection intervals.

U2 - 10.1190/segam2013-0830.1

DO - 10.1190/segam2013-0830.1

M3 - Conference contribution

SP - 2013

EP - 2018

BT - SEG Technical Program Expanded Abstracts 2013

PB - Society of Exploration Geophysicists

ER -

ID: 4736592