Research output: Contribution to journal › Article › peer-review
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 et al.
In: International Geology Review, Vol. 65, No. 15, 2023, p. 2426-2446.Research output: Contribution to journal › Article › peer-review
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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
N1 - Publisher Copyright: © 2022 Informa UK Limited, trading as Taylor & Francis Group.
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