Standard

Active Faults and Late Holocene Surface Rupturing Earthquakes in the Kokorya Basin (Gorny Altai, Russia). / Deev, E. V.; Krzhivoblotskaya, V. E.; Borodovskiy, A. P. et al.

In: Doklady Earth Sciences, Vol. 506, No. 1, 09.2022, p. 666-670.

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

Harvard

Deev, EV, Krzhivoblotskaya, VE, Borodovskiy, AP & Entin, AL 2022, 'Active Faults and Late Holocene Surface Rupturing Earthquakes in the Kokorya Basin (Gorny Altai, Russia)', Doklady Earth Sciences, vol. 506, no. 1, pp. 666-670. https://doi.org/10.1134/S1028334X22700039

APA

Deev, E. V., Krzhivoblotskaya, V. E., Borodovskiy, A. P., & Entin, A. L. (2022). Active Faults and Late Holocene Surface Rupturing Earthquakes in the Kokorya Basin (Gorny Altai, Russia). Doklady Earth Sciences, 506(1), 666-670. https://doi.org/10.1134/S1028334X22700039

Vancouver

Deev EV, Krzhivoblotskaya VE, Borodovskiy AP, Entin AL. Active Faults and Late Holocene Surface Rupturing Earthquakes in the Kokorya Basin (Gorny Altai, Russia). Doklady Earth Sciences. 2022 Sept;506(1):666-670. doi: 10.1134/S1028334X22700039

Author

Deev, E. V. ; Krzhivoblotskaya, V. E. ; Borodovskiy, A. P. et al. / Active Faults and Late Holocene Surface Rupturing Earthquakes in the Kokorya Basin (Gorny Altai, Russia). In: Doklady Earth Sciences. 2022 ; Vol. 506, No. 1. pp. 666-670.

BibTeX

@article{69ebf7a26ad548c4a3032c75678aab79,
title = "Active Faults and Late Holocene Surface Rupturing Earthquakes in the Kokorya Basin (Gorny Altai, Russia)",
abstract = "A system of 22 km long surface rupture produced by paleoearthquakes has been mapped for the first time along the Kubadru Fault which delineates the Kokorya Basin in the north. The ruptures morphology record reverse and right-lateral strike-slip geometry of the Kubadru Fault. The ruptures pattern represent a combined effect of four paleoearthquakes, including three events in the past 1.4 kyr. The magnitudes of the earthquakes could range from 6.7 to 7.6. The revealed structure of the Kubadru Fault Zone consists of counter-dipping reverse faults. Motions on two reverse fault systems maintained thrusting of the Kurai Range on the basin sediments and caused the growth of a foreberg between the basin and the range.",
keywords = "active fault, Gorny Altai, Kokorya Basin, Kubadru Fault, large paleoearthquake",
author = "Deev, {E. V.} and Krzhivoblotskaya, {V. E.} and Borodovskiy, {A. P.} and Entin, {A. L.}",
note = "Funding Information: The work was supported by the Russian Science Foundation: Project 21-17-00058. Drone Geoscan Gemini, software Agisoft Metahsape 1.7, and equipment for processing aerial images were provided by the Center of Collective Usage “Geoportal MGU.” Publisher Copyright: {\textcopyright} 2022, Pleiades Publishing, Ltd.",
year = "2022",
month = sep,
doi = "10.1134/S1028334X22700039",
language = "English",
volume = "506",
pages = "666--670",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "1",

}

RIS

TY - JOUR

T1 - Active Faults and Late Holocene Surface Rupturing Earthquakes in the Kokorya Basin (Gorny Altai, Russia)

AU - Deev, E. V.

AU - Krzhivoblotskaya, V. E.

AU - Borodovskiy, A. P.

AU - Entin, A. L.

N1 - Funding Information: The work was supported by the Russian Science Foundation: Project 21-17-00058. Drone Geoscan Gemini, software Agisoft Metahsape 1.7, and equipment for processing aerial images were provided by the Center of Collective Usage “Geoportal MGU.” Publisher Copyright: © 2022, Pleiades Publishing, Ltd.

PY - 2022/9

Y1 - 2022/9

N2 - A system of 22 km long surface rupture produced by paleoearthquakes has been mapped for the first time along the Kubadru Fault which delineates the Kokorya Basin in the north. The ruptures morphology record reverse and right-lateral strike-slip geometry of the Kubadru Fault. The ruptures pattern represent a combined effect of four paleoearthquakes, including three events in the past 1.4 kyr. The magnitudes of the earthquakes could range from 6.7 to 7.6. The revealed structure of the Kubadru Fault Zone consists of counter-dipping reverse faults. Motions on two reverse fault systems maintained thrusting of the Kurai Range on the basin sediments and caused the growth of a foreberg between the basin and the range.

AB - A system of 22 km long surface rupture produced by paleoearthquakes has been mapped for the first time along the Kubadru Fault which delineates the Kokorya Basin in the north. The ruptures morphology record reverse and right-lateral strike-slip geometry of the Kubadru Fault. The ruptures pattern represent a combined effect of four paleoearthquakes, including three events in the past 1.4 kyr. The magnitudes of the earthquakes could range from 6.7 to 7.6. The revealed structure of the Kubadru Fault Zone consists of counter-dipping reverse faults. Motions on two reverse fault systems maintained thrusting of the Kurai Range on the basin sediments and caused the growth of a foreberg between the basin and the range.

KW - active fault

KW - Gorny Altai

KW - Kokorya Basin

KW - Kubadru Fault

KW - large paleoearthquake

UR - http://www.scopus.com/inward/record.url?scp=85138752830&partnerID=8YFLogxK

UR - https://www.mendeley.com/catalogue/b92ba3fd-491c-3902-90c0-155ab61faf6d/

U2 - 10.1134/S1028334X22700039

DO - 10.1134/S1028334X22700039

M3 - Article

AN - SCOPUS:85138752830

VL - 506

SP - 666

EP - 670

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 38046648