Large Holocene paleoseismic events and synchronized travertine formation: a case study of the Kurai fault zone (Gorny Altai, Russia)

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Large Holocene paleoseismic events and synchronized travertine formation: a case study of the Kurai fault zone (Gorny Altai, Russia). / Deev, Evgeny ; Dublyansky, Yuri ; Kokh, Svetlana и др.

в: International Geology Review, Том 65, № 15, 2023, стр. 2426-2446.

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

BibTeX

@article{21d77726285d4ee59289399a1cdddbca,

title = "Large Holocene paleoseismic events and synchronized travertine formation: a case study of the Kurai fault zone (Gorny Altai, Russia)",

abstract = "The Kurai Fault Zone (KFZ) is one of the most hazardous seismogenic structures in the Gorny Altai (Russia), which bounds the largest Kurai and Chuya intermontane basins from the north. Trenching studies, radiocarbon dating of colluvial wedge deposits, and 230Th-U dating of seismogenic travertine of the Meshtuyaryk field showed that the fault scarp in the northwestern part of the Chuya Depression was formed by earthquakes that occurred ca. 9.5, 7.7, 5.8, and 4.8–3.4 ka BP. The last two palaeoearthquakes are younger than 3.2 ka BP. The parameters of seismogenic ruptures, as well as the distances between coeval seismogenic travertines along the KFZ, yielded estimates of the Mw of the four oldest palaeoearthquakes as 6.8–7.6 and ESI 2007 shaking intensities of VIII–XI. The results of 230Th-U dating suggest that deposition of the Meshtuyaryk travertines was triggered by three strong palaeoearthquakes at ca. 9.5, 7.7, and 4.8–3.4 ka BP, which activated faults and caused a rapid rise along them of ambient-temperature bicarbonate groundwaters previously sealed in deep-seated limestone aquifers.",

keywords = "Th-U dating, active fault, Gorny Altai, Large palaeoearthquke, travertine, 230Th-U dating",

author = "Evgeny Deev and Yuri Dublyansky and Svetlana Kokh and Denis Scholz and Gennady Rusanov and Ella Sokol and Pavel Khvorov and Vadim Reutsky and Andrey Panin",

note = "Publisher Copyright: {\textcopyright} 2022 Informa UK Limited, trading as Taylor & Francis Group.",

year = "2023",

doi = "10.1080/00206814.2022.2145510",

language = "English",

volume = "65",

pages = "2426--2446",

journal = "International Geology Review",

issn = "0020-6814",

publisher = "Taylor and Francis Ltd.",

number = "15",

}

RIS

TY - JOUR

T1 - Large Holocene paleoseismic events and synchronized travertine formation: a case study of the Kurai fault zone (Gorny Altai, Russia)

AU - Deev, Evgeny

AU - Dublyansky, Yuri

AU - Kokh, Svetlana

AU - Scholz, Denis

AU - Rusanov, Gennady

AU - Sokol, Ella

AU - Khvorov, Pavel

AU - Reutsky, Vadim

AU - Panin, Andrey

PY - 2023

Y1 - 2023

N2 - The Kurai Fault Zone (KFZ) is one of the most hazardous seismogenic structures in the Gorny Altai (Russia), which bounds the largest Kurai and Chuya intermontane basins from the north. Trenching studies, radiocarbon dating of colluvial wedge deposits, and 230Th-U dating of seismogenic travertine of the Meshtuyaryk field showed that the fault scarp in the northwestern part of the Chuya Depression was formed by earthquakes that occurred ca. 9.5, 7.7, 5.8, and 4.8–3.4 ka BP. The last two palaeoearthquakes are younger than 3.2 ka BP. The parameters of seismogenic ruptures, as well as the distances between coeval seismogenic travertines along the KFZ, yielded estimates of the Mw of the four oldest palaeoearthquakes as 6.8–7.6 and ESI 2007 shaking intensities of VIII–XI. The results of 230Th-U dating suggest that deposition of the Meshtuyaryk travertines was triggered by three strong palaeoearthquakes at ca. 9.5, 7.7, and 4.8–3.4 ka BP, which activated faults and caused a rapid rise along them of ambient-temperature bicarbonate groundwaters previously sealed in deep-seated limestone aquifers.

AB - The Kurai Fault Zone (KFZ) is one of the most hazardous seismogenic structures in the Gorny Altai (Russia), which bounds the largest Kurai and Chuya intermontane basins from the north. Trenching studies, radiocarbon dating of colluvial wedge deposits, and 230Th-U dating of seismogenic travertine of the Meshtuyaryk field showed that the fault scarp in the northwestern part of the Chuya Depression was formed by earthquakes that occurred ca. 9.5, 7.7, 5.8, and 4.8–3.4 ka BP. The last two palaeoearthquakes are younger than 3.2 ka BP. The parameters of seismogenic ruptures, as well as the distances between coeval seismogenic travertines along the KFZ, yielded estimates of the Mw of the four oldest palaeoearthquakes as 6.8–7.6 and ESI 2007 shaking intensities of VIII–XI. The results of 230Th-U dating suggest that deposition of the Meshtuyaryk travertines was triggered by three strong palaeoearthquakes at ca. 9.5, 7.7, and 4.8–3.4 ka BP, which activated faults and caused a rapid rise along them of ambient-temperature bicarbonate groundwaters previously sealed in deep-seated limestone aquifers.

KW - Th-U dating

KW - active fault

KW - Gorny Altai

KW - Large palaeoearthquke

KW - travertine

KW - 230Th-U dating

UR - http://www.scopus.com/inward/record.url?scp=85142871238&partnerID=8YFLogxK

UR - https://www.mendeley.com/catalogue/fa5301a8-84f6-35b1-a753-d4cd5b70259d/

U2 - 10.1080/00206814.2022.2145510

DO - 10.1080/00206814.2022.2145510

M3 - Article

AN - SCOPUS:85142871238

VL - 65

SP - 2426

EP - 2446

JO - International Geology Review

JF - International Geology Review

SN - 0020-6814

IS - 15

ER -

ID: 40097433