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Prestack Depth Migration and Velocity Model Derived from First Break Tomography at Long Offsets. / Roslov, Y.V.; Polovkov, V.V.

2010. Paper presented at 4th EAGE St.Petersburg International Conference and Exhibition on Geosciences - New Discoveries through Integration of Geosciences.

Research output: Contribution to conferencePaper

Harvard

Roslov, YV & Polovkov, VV 2010, 'Prestack Depth Migration and Velocity Model Derived from First Break Tomography at Long Offsets', Paper presented at 4th EAGE St.Petersburg International Conference and Exhibition on Geosciences - New Discoveries through Integration of Geosciences, 4/05/10 - 6/05/10. <http://earthdoc.eage.org/publication/publicationdetails/?publication=38535>

APA

Roslov, Y. V., & Polovkov, V. V. (2010). Prestack Depth Migration and Velocity Model Derived from First Break Tomography at Long Offsets. Paper presented at 4th EAGE St.Petersburg International Conference and Exhibition on Geosciences - New Discoveries through Integration of Geosciences. http://earthdoc.eage.org/publication/publicationdetails/?publication=38535

Vancouver

Roslov YV, Polovkov VV. Prestack Depth Migration and Velocity Model Derived from First Break Tomography at Long Offsets. 2010. Paper presented at 4th EAGE St.Petersburg International Conference and Exhibition on Geosciences - New Discoveries through Integration of Geosciences.

Author

Roslov, Y.V. ; Polovkov, V.V. / Prestack Depth Migration and Velocity Model Derived from First Break Tomography at Long Offsets. Paper presented at 4th EAGE St.Petersburg International Conference and Exhibition on Geosciences - New Discoveries through Integration of Geosciences.

BibTeX

@conference{ad4c7926d6a5438b9868d33413de012d,
title = "Prestack Depth Migration and Velocity Model Derived from First Break Tomography at Long Offsets",
abstract = "First break tomography at long offsets is used to build up velocity model for prestack depth migration. Processing of refracted and diving waves forming first breaks allows obtaining of velocity information in complex geological structures where reflection seismic fails. That, first of all, concern cases of smooth velocity anomalies which are not related with horizons. The advantage of the approach proposed is demonstrated at test models and Pechora Sea survey where multichannel seismic data and wide angle profiling data were acquired independently along one line. Velocity model derived from first break tomography of wide angle data was used for multichannel data prestack depth migration. The final seismic image is compared with ones obtained with standard algorithms)",
author = "Y.V. Roslov and V.V. Polovkov",
year = "2010",
language = "English",
note = "null ; Conference date: 04-05-2010 Through 06-05-2010",
url = "https://www.earthdoc.org/content/proceedings/saintpetersburg2010",

}

RIS

TY - CONF

T1 - Prestack Depth Migration and Velocity Model Derived from First Break Tomography at Long Offsets

AU - Roslov, Y.V.

AU - Polovkov, V.V.

PY - 2010

Y1 - 2010

N2 - First break tomography at long offsets is used to build up velocity model for prestack depth migration. Processing of refracted and diving waves forming first breaks allows obtaining of velocity information in complex geological structures where reflection seismic fails. That, first of all, concern cases of smooth velocity anomalies which are not related with horizons. The advantage of the approach proposed is demonstrated at test models and Pechora Sea survey where multichannel seismic data and wide angle profiling data were acquired independently along one line. Velocity model derived from first break tomography of wide angle data was used for multichannel data prestack depth migration. The final seismic image is compared with ones obtained with standard algorithms)

AB - First break tomography at long offsets is used to build up velocity model for prestack depth migration. Processing of refracted and diving waves forming first breaks allows obtaining of velocity information in complex geological structures where reflection seismic fails. That, first of all, concern cases of smooth velocity anomalies which are not related with horizons. The advantage of the approach proposed is demonstrated at test models and Pechora Sea survey where multichannel seismic data and wide angle profiling data were acquired independently along one line. Velocity model derived from first break tomography of wide angle data was used for multichannel data prestack depth migration. The final seismic image is compared with ones obtained with standard algorithms)

M3 - Paper

Y2 - 4 May 2010 through 6 May 2010

ER -

ID: 103204911