Standard

Fault kinematics and paleostress analysis using seismic data : A case study from the Archinsk field, West Siberian Basin, Russia. / Moskalenko, Artem; Khudoley, Andrey; Cardozo, Nestor.

In: Journal of Structural Geology, Vol. 141, 104194, 12.2020.

Research output: Contribution to journal › Article › peer-review

Harvard

Moskalenko, A, Khudoley, A & Cardozo, N 2020, 'Fault kinematics and paleostress analysis using seismic data: A case study from the Archinsk field, West Siberian Basin, Russia', Journal of Structural Geology, vol. 141, 104194. https://doi.org/10.1016/j.jsg.2020.104194

APA

Moskalenko, A., Khudoley, A., & Cardozo, N. (2020). Fault kinematics and paleostress analysis using seismic data: A case study from the Archinsk field, West Siberian Basin, Russia. Journal of Structural Geology, 141, [104194]. https://doi.org/10.1016/j.jsg.2020.104194

Vancouver

Moskalenko A, Khudoley A, Cardozo N. Fault kinematics and paleostress analysis using seismic data: A case study from the Archinsk field, West Siberian Basin, Russia. Journal of Structural Geology. 2020 Dec;141. 104194. https://doi.org/10.1016/j.jsg.2020.104194

Author

Moskalenko, Artem ; Khudoley, Andrey ; Cardozo, Nestor. / Fault kinematics and paleostress analysis using seismic data : A case study from the Archinsk field, West Siberian Basin, Russia. In: Journal of Structural Geology. 2020 ; Vol. 141.

BibTeX

@article{f601491ce0474edc892c095c308fadb3,
title = "Fault kinematics and paleostress analysis using seismic data: A case study from the Archinsk field, West Siberian Basin, Russia",
abstract = "We present a methodology to determine the stress field based on the analysis of 3D seismic reflection data without additional information from wells. It involves the analysis of seismic horizons that were folded before the analyzed fault system. Fold hinges-faults intersections provide piercing points and fault slip vectors, which can be processed in the same way as slickenlines. Four seismic horizons and 51 faults in the Archinsk field, West Siberian Basin, were analyzed. The resulting fault-slip dataset is heterogeneous and has 126 slip vectors, corresponding to normal and strike-slip faulting. A normal stress regime with stress ratio (Φ) of 0.5 and a NE-trending minimum principal stress (σ3) is identified for the Late Triassic-Early Jurassic. A strike-slip stress regime with stress ratio (Φ) of 0.3, NW- and NE-trending maximum (σ1) and minimum principal stresses (σ3) corresponds to the present-day stress field.",
keywords = "3D seismic, Archinsk field, Fault kinematics, Paleostress, West Siberian Basin",
author = "Artem Moskalenko and Andrey Khudoley and Nestor Cardozo",
note = "Publisher Copyright: {\textcopyright} 2020 Elsevier Ltd",
year = "2020",
month = dec,
doi = "10.1016/j.jsg.2020.104194",
language = "English",
volume = "141",
journal = "Journal of Structural Geology",
issn = "0191-8141",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - Fault kinematics and paleostress analysis using seismic data

T2 - A case study from the Archinsk field, West Siberian Basin, Russia

AU - Moskalenko, Artem

AU - Khudoley, Andrey

AU - Cardozo, Nestor

N1 - Publisher Copyright: © 2020 Elsevier Ltd

PY - 2020/12

Y1 - 2020/12

N2 - We present a methodology to determine the stress field based on the analysis of 3D seismic reflection data without additional information from wells. It involves the analysis of seismic horizons that were folded before the analyzed fault system. Fold hinges-faults intersections provide piercing points and fault slip vectors, which can be processed in the same way as slickenlines. Four seismic horizons and 51 faults in the Archinsk field, West Siberian Basin, were analyzed. The resulting fault-slip dataset is heterogeneous and has 126 slip vectors, corresponding to normal and strike-slip faulting. A normal stress regime with stress ratio (Φ) of 0.5 and a NE-trending minimum principal stress (σ3) is identified for the Late Triassic-Early Jurassic. A strike-slip stress regime with stress ratio (Φ) of 0.3, NW- and NE-trending maximum (σ1) and minimum principal stresses (σ3) corresponds to the present-day stress field.

AB - We present a methodology to determine the stress field based on the analysis of 3D seismic reflection data without additional information from wells. It involves the analysis of seismic horizons that were folded before the analyzed fault system. Fold hinges-faults intersections provide piercing points and fault slip vectors, which can be processed in the same way as slickenlines. Four seismic horizons and 51 faults in the Archinsk field, West Siberian Basin, were analyzed. The resulting fault-slip dataset is heterogeneous and has 126 slip vectors, corresponding to normal and strike-slip faulting. A normal stress regime with stress ratio (Φ) of 0.5 and a NE-trending minimum principal stress (σ3) is identified for the Late Triassic-Early Jurassic. A strike-slip stress regime with stress ratio (Φ) of 0.3, NW- and NE-trending maximum (σ1) and minimum principal stresses (σ3) corresponds to the present-day stress field.

KW - 3D seismic

KW - Archinsk field

KW - Fault kinematics

KW - Paleostress

KW - West Siberian Basin

UR - http://www.scopus.com/inward/record.url?scp=85092368992&partnerID=8YFLogxK

U2 - 10.1016/j.jsg.2020.104194

DO - 10.1016/j.jsg.2020.104194

M3 - Article

AN - SCOPUS:85092368992

VL - 141

JO - Journal of Structural Geology

JF - Journal of Structural Geology

SN - 0191-8141

M1 - 104194

ER -

ID: 89180327