Standard

Seismic imaging and statistical analysis of fault facies models. / Kolyukhin, Dmitriy R.; Lisitsa, Vadim V.; Protasov, Maxim I. и др.

в: Interpretation, Том 5, № 4, 30.11.2017, стр. SP71-SP82.

Результаты исследований: Научные публикации в периодических изданияхстатьяРецензирование

Harvard

Kolyukhin, DR, Lisitsa, VV, Protasov, MI, Qu, D, Reshetova, GV, Tveranger, J, Tcheverda, VA & Vishnevsky, DM 2017, 'Seismic imaging and statistical analysis of fault facies models', Interpretation, Том. 5, № 4, стр. SP71-SP82. https://doi.org/10.1190/INT-2016-0202.1

APA

Kolyukhin, D. R., Lisitsa, V. V., Protasov, M. I., Qu, D., Reshetova, G. V., Tveranger, J., Tcheverda, V. A., & Vishnevsky, D. M. (2017). Seismic imaging and statistical analysis of fault facies models. Interpretation, 5(4), SP71-SP82. https://doi.org/10.1190/INT-2016-0202.1

Vancouver

Kolyukhin DR, Lisitsa VV, Protasov MI, Qu D, Reshetova GV, Tveranger J и др. Seismic imaging and statistical analysis of fault facies models. Interpretation. 2017 нояб. 30;5(4):SP71-SP82. doi: 10.1190/INT-2016-0202.1

Author

Kolyukhin, Dmitriy R. ; Lisitsa, Vadim V. ; Protasov, Maxim I. и др. / Seismic imaging and statistical analysis of fault facies models. в: Interpretation. 2017 ; Том 5, № 4. стр. SP71-SP82.

BibTeX

@article{5d718b88ebe34f44a8ad371b694c24ae,
title = "Seismic imaging and statistical analysis of fault facies models",
abstract = "Interpretation of seismic responses from subsurface fault zones is hampered by the fact that the geologic structure and property distributions of fault zones can generally not be directly observed. This shortcoming curtails the use of seismic data for characterizing internal structure and properties of fault zones, and it has instead promoted the use of interpretation techniques that tend to simplify actual structural complexity by rendering faults as lines and planes rather than volumes of deformed rock. Facilitating the correlation of rock properties and seismic images of fault zones would enable active use of these images for interpreting fault zones, which in turn would improve our ability to assess the impact of fault zones on subsurface fluid flow. We use a combination of 3D fault zone models, based on empirical data and 2D forward seismic modeling to investigate the link between fault zone properties and seismic response. A comparison of spatial statistics from the geologic models and the seismic images was carried out to study how well seismic images render the modeled geologic features. Our results indicate the feasibility of extracting information about fault zone structure from seismic data by the methods used.",
keywords = "facies, faults, imaging, seismic impedance, statistics, POROSITY, FLUID-FLOW, POROUS SANDSTONES, HETEROGENEOUS MEDIA, WAVE PROPAGATION, SIMULATION, DAMAGE ZONE, DEFORMATION BANDS, SPATIAL-DISTRIBUTION, RESERVOIR MODELS",
author = "Kolyukhin, {Dmitriy R.} and Lisitsa, {Vadim V.} and Protasov, {Maxim I.} and Dongfang Qu and Reshetova, {Galina V.} and Jan Tveranger and Tcheverda, {Vladimir A.} and Vishnevsky, {Dmitry M.}",
year = "2017",
month = nov,
day = "30",
doi = "10.1190/INT-2016-0202.1",
language = "English",
volume = "5",
pages = "SP71--SP82",
journal = "Interpretation",
issn = "2324-8858",
publisher = "Society of Exploration Geophysicists",
number = "4",

}

RIS

TY - JOUR

T1 - Seismic imaging and statistical analysis of fault facies models

AU - Kolyukhin, Dmitriy R.

AU - Lisitsa, Vadim V.

AU - Protasov, Maxim I.

AU - Qu, Dongfang

AU - Reshetova, Galina V.

AU - Tveranger, Jan

AU - Tcheverda, Vladimir A.

AU - Vishnevsky, Dmitry M.

PY - 2017/11/30

Y1 - 2017/11/30

N2 - Interpretation of seismic responses from subsurface fault zones is hampered by the fact that the geologic structure and property distributions of fault zones can generally not be directly observed. This shortcoming curtails the use of seismic data for characterizing internal structure and properties of fault zones, and it has instead promoted the use of interpretation techniques that tend to simplify actual structural complexity by rendering faults as lines and planes rather than volumes of deformed rock. Facilitating the correlation of rock properties and seismic images of fault zones would enable active use of these images for interpreting fault zones, which in turn would improve our ability to assess the impact of fault zones on subsurface fluid flow. We use a combination of 3D fault zone models, based on empirical data and 2D forward seismic modeling to investigate the link between fault zone properties and seismic response. A comparison of spatial statistics from the geologic models and the seismic images was carried out to study how well seismic images render the modeled geologic features. Our results indicate the feasibility of extracting information about fault zone structure from seismic data by the methods used.

AB - Interpretation of seismic responses from subsurface fault zones is hampered by the fact that the geologic structure and property distributions of fault zones can generally not be directly observed. This shortcoming curtails the use of seismic data for characterizing internal structure and properties of fault zones, and it has instead promoted the use of interpretation techniques that tend to simplify actual structural complexity by rendering faults as lines and planes rather than volumes of deformed rock. Facilitating the correlation of rock properties and seismic images of fault zones would enable active use of these images for interpreting fault zones, which in turn would improve our ability to assess the impact of fault zones on subsurface fluid flow. We use a combination of 3D fault zone models, based on empirical data and 2D forward seismic modeling to investigate the link between fault zone properties and seismic response. A comparison of spatial statistics from the geologic models and the seismic images was carried out to study how well seismic images render the modeled geologic features. Our results indicate the feasibility of extracting information about fault zone structure from seismic data by the methods used.

KW - facies

KW - faults

KW - imaging

KW - seismic impedance

KW - statistics

KW - POROSITY

KW - FLUID-FLOW

KW - POROUS SANDSTONES

KW - HETEROGENEOUS MEDIA

KW - WAVE PROPAGATION

KW - SIMULATION

KW - DAMAGE ZONE

KW - DEFORMATION BANDS

KW - SPATIAL-DISTRIBUTION

KW - RESERVOIR MODELS

UR - http://www.scopus.com/inward/record.url?scp=85029117136&partnerID=8YFLogxK

U2 - 10.1190/INT-2016-0202.1

DO - 10.1190/INT-2016-0202.1

M3 - Article

AN - SCOPUS:85029117136

VL - 5

SP - SP71-SP82

JO - Interpretation

JF - Interpretation

SN - 2324-8858

IS - 4

ER -

ID: 25775110