Results of studying the azimuthal anisotropy of the paleozoic basement with vsp technique at the Bystrovka vibroseismic test site
https://doi.org/10.18303/2619-1563-2021-1-19
Abstract
At the Bystrovka vibroseismic test site (Novosibirsk region) 3-component refracted waves profiling was performed at three intersecting lines. Shear waves analysis made possible to detect anisotropy of the Paleozoic basement occurring at depth of about 10 m and to suggest symmetry elements of this medium along with their orientation. Compressional waves data were used to construct depth sections estimating head waves velocities. These velocities demonstrate significant variation in lines of different orientation. The results obtained agree with previously performed VSP.
About the Authors
S. B. Gorshkalev
Trofimuk Institute of Petroleum Geology and Geophysics SB RAS, Koptyug Ave., 3, Novosibirsk, 630090
Russian Federation
Russian Federation
V. V. Karsten
Trofimuk Institute of Petroleum Geology and Geophysics SB RAS, Koptyug Ave., 3, Novosibirsk, 630090
Russian Federation
Russian Federation
P. A. Dergach
Trofimuk Institute of Petroleum Geology and Geophysics SB RAS, Koptyug Ave., 3, Novosibirsk, 630090
Russian Federation
Russian Federation
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Review
For citations:
Gorshkalev S.B., Karsten V.V., Dergach P.A. Results of studying the azimuthal anisotropy of the paleozoic basement with vsp technique at the Bystrovka vibroseismic test site. Russian Journal of Geophysical Technologies. 2021;(1):19-37. (In Russ.) https://doi.org/10.18303/2619-1563-2021-1-19
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