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The Geodynamics of the Katun Fault (Gorny Altai) according to Structural and Kinematic Data. / Tveritinova, T. Yu; Marinin, A. V.; Deev, E. V.

в: Moscow University Geology Bulletin, Том 78, № 2, 04.2023, стр. 225-238.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Tveritinova, TY, Marinin, AV & Deev, EV 2023, 'The Geodynamics of the Katun Fault (Gorny Altai) according to Structural and Kinematic Data', Moscow University Geology Bulletin, Том. 78, № 2, стр. 225-238. https://doi.org/10.3103/S0145875223020126

APA

Tveritinova, T. Y., Marinin, A. V., & Deev, E. V. (2023). The Geodynamics of the Katun Fault (Gorny Altai) according to Structural and Kinematic Data. Moscow University Geology Bulletin, 78(2), 225-238. https://doi.org/10.3103/S0145875223020126

Vancouver

Tveritinova TY, Marinin AV, Deev EV. The Geodynamics of the Katun Fault (Gorny Altai) according to Structural and Kinematic Data. Moscow University Geology Bulletin. 2023 апр.;78(2):225-238. doi: 10.3103/S0145875223020126

Author

Tveritinova, T. Yu ; Marinin, A. V. ; Deev, E. V. / The Geodynamics of the Katun Fault (Gorny Altai) according to Structural and Kinematic Data. в: Moscow University Geology Bulletin. 2023 ; Том 78, № 2. стр. 225-238.

BibTeX

@article{03966b21b55843258151a5ef23db4710,
title = "The Geodynamics of the Katun Fault (Gorny Altai) according to Structural and Kinematic Data",
abstract = "The kinematic characteristics of faults included in the structure of the active Katun Fault in Gorny Altai have been determined by methods of structural–paragenetic and cataclastic analysis of disjunctives (faults). It is proven that the Katun Fault is a strike-slip fault developing in different areas under transpressive or transtensional conditions. The most recent grabens along the Katun fault were formed under conditions of strike-slip displacements and locally manifested horizontal extension or extension with shear.",
keywords = "Gorny Altai, Katun Fault, cleavages, faults, fractures, grabens, ruptures, slickensides, veins",
author = "Tveritinova, {T. Yu} and Marinin, {A. V.} and Deev, {E. V.}",
note = "This study was carried out according to the State Assignments of the Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, and Institute of Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Sciences. Публикация для корректировки.",
year = "2023",
month = apr,
doi = "10.3103/S0145875223020126",
language = "English",
volume = "78",
pages = "225--238",
journal = "Moscow University Geology Bulletin",
issn = "1934-8436",
publisher = "Pleiades Publishing",
number = "2",

}

RIS

TY - JOUR

T1 - The Geodynamics of the Katun Fault (Gorny Altai) according to Structural and Kinematic Data

AU - Tveritinova, T. Yu

AU - Marinin, A. V.

AU - Deev, E. V.

N1 - This study was carried out according to the State Assignments of the Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, and Institute of Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Sciences. Публикация для корректировки.

PY - 2023/4

Y1 - 2023/4

N2 - The kinematic characteristics of faults included in the structure of the active Katun Fault in Gorny Altai have been determined by methods of structural–paragenetic and cataclastic analysis of disjunctives (faults). It is proven that the Katun Fault is a strike-slip fault developing in different areas under transpressive or transtensional conditions. The most recent grabens along the Katun fault were formed under conditions of strike-slip displacements and locally manifested horizontal extension or extension with shear.

AB - The kinematic characteristics of faults included in the structure of the active Katun Fault in Gorny Altai have been determined by methods of structural–paragenetic and cataclastic analysis of disjunctives (faults). It is proven that the Katun Fault is a strike-slip fault developing in different areas under transpressive or transtensional conditions. The most recent grabens along the Katun fault were formed under conditions of strike-slip displacements and locally manifested horizontal extension or extension with shear.

KW - Gorny Altai

KW - Katun Fault

KW - cleavages

KW - faults

KW - fractures

KW - grabens

KW - ruptures

KW - slickensides

KW - veins

UR - https://www.scopus.com/record/display.uri?eid=2-s2.0-85169599135&origin=inward&txGid=69b4859e67e443e1e4a92caa9ddd49cc

UR - https://www.mendeley.com/catalogue/f5d9c997-5e7c-34f7-86a7-d253b351f5b4/

U2 - 10.3103/S0145875223020126

DO - 10.3103/S0145875223020126

M3 - Article

VL - 78

SP - 225

EP - 238

JO - Moscow University Geology Bulletin

JF - Moscow University Geology Bulletin

SN - 1934-8436

IS - 2

ER -

ID: 59647233