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230Th/U Dating of Travertines Related to Paleoearthquakes in Gorny Altai: First Results. / Deev, E. V.; Dublyansky, Y. V.; Pozdnyakova, N. I. и др.

в: Doklady Earth Sciences, Том 500, № 2, 10.2021, стр. 820-825.

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

Harvard

Deev, EV, Dublyansky, YV, Pozdnyakova, NI, Scholz, D, Kokh, SN, Sokol, EV & Rusanov, GG 2021, '230Th/U Dating of Travertines Related to Paleoearthquakes in Gorny Altai: First Results', Doklady Earth Sciences, Том. 500, № 2, стр. 820-825. https://doi.org/10.1134/S1028334X21100081

APA

Deev, E. V., Dublyansky, Y. V., Pozdnyakova, N. I., Scholz, D., Kokh, S. N., Sokol, E. V., & Rusanov, G. G. (2021). 230Th/U Dating of Travertines Related to Paleoearthquakes in Gorny Altai: First Results. Doklady Earth Sciences, 500(2), 820-825. https://doi.org/10.1134/S1028334X21100081

Vancouver

Deev EV, Dublyansky YV, Pozdnyakova NI, Scholz D, Kokh SN, Sokol EV и др. 230Th/U Dating of Travertines Related to Paleoearthquakes in Gorny Altai: First Results. Doklady Earth Sciences. 2021 окт.;500(2):820-825. doi: 10.1134/S1028334X21100081

Author

Deev, E. V. ; Dublyansky, Y. V. ; Pozdnyakova, N. I. и др. / 230Th/U Dating of Travertines Related to Paleoearthquakes in Gorny Altai: First Results. в: Doklady Earth Sciences. 2021 ; Том 500, № 2. стр. 820-825.

BibTeX

@article{c8537fa2a20f4186a9dee409480dbbcd,
title = "230Th/U Dating of Travertines Related to Paleoearthquakes in Gorny Altai: First Results",
abstract = "First 230Th/U-dating results have been obtained for six Quaternary travertine deposits from the southeastern Gorny Altai associated with zones of active faults that bound the Chuya and Kurai intermontane basins. The travertines consist mainly of calcite (with minor aragonite), which cements alluvial, alluvial fan, and colluvial deposits. The travertines dated at 1.3, 4.9, and 6.3 ka BP were related to large (Mw = 6.5–6.9) paleoearthquakes. The age of an 11 ka BP travertine falls into the 8.5 to 16 ka BP interval of high seismicity in the region. The 123 ka BP travertine results from slip triggered by the Middle Pleistocene deglaciation, while that of 400 ka BP represents seismic motions during the main Cenozoic orogenic phase.",
keywords = "Th/U geochronology, active fault, Gorny Altai, large paleoearthquake, travertine",
author = "Deev, {E. V.} and Dublyansky, {Y. V.} and Pozdnyakova, {N. I.} and D. Scholz and Kokh, {S. N.} and Sokol, {E. V.} and Rusanov, {G. G.}",
note = "Funding Information: The work was supported by the Russian Science Foundation: Project 19-17-00179 for paleoseismological research and Project 21-17-00058 for the studies of travertines. Publisher Copyright: {\textcopyright} 2021, Pleiades Publishing, Ltd.",
year = "2021",
month = oct,
doi = "10.1134/S1028334X21100081",
language = "English",
volume = "500",
pages = "820--825",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - 230Th/U Dating of Travertines Related to Paleoearthquakes in Gorny Altai: First Results

AU - Deev, E. V.

AU - Dublyansky, Y. V.

AU - Pozdnyakova, N. I.

AU - Scholz, D.

AU - Kokh, S. N.

AU - Sokol, E. V.

AU - Rusanov, G. G.

N1 - Funding Information: The work was supported by the Russian Science Foundation: Project 19-17-00179 for paleoseismological research and Project 21-17-00058 for the studies of travertines. Publisher Copyright: © 2021, Pleiades Publishing, Ltd.

PY - 2021/10

Y1 - 2021/10

N2 - First 230Th/U-dating results have been obtained for six Quaternary travertine deposits from the southeastern Gorny Altai associated with zones of active faults that bound the Chuya and Kurai intermontane basins. The travertines consist mainly of calcite (with minor aragonite), which cements alluvial, alluvial fan, and colluvial deposits. The travertines dated at 1.3, 4.9, and 6.3 ka BP were related to large (Mw = 6.5–6.9) paleoearthquakes. The age of an 11 ka BP travertine falls into the 8.5 to 16 ka BP interval of high seismicity in the region. The 123 ka BP travertine results from slip triggered by the Middle Pleistocene deglaciation, while that of 400 ka BP represents seismic motions during the main Cenozoic orogenic phase.

AB - First 230Th/U-dating results have been obtained for six Quaternary travertine deposits from the southeastern Gorny Altai associated with zones of active faults that bound the Chuya and Kurai intermontane basins. The travertines consist mainly of calcite (with minor aragonite), which cements alluvial, alluvial fan, and colluvial deposits. The travertines dated at 1.3, 4.9, and 6.3 ka BP were related to large (Mw = 6.5–6.9) paleoearthquakes. The age of an 11 ka BP travertine falls into the 8.5 to 16 ka BP interval of high seismicity in the region. The 123 ka BP travertine results from slip triggered by the Middle Pleistocene deglaciation, while that of 400 ka BP represents seismic motions during the main Cenozoic orogenic phase.

KW - Th/U geochronology

KW - active fault

KW - Gorny Altai

KW - large paleoearthquake

KW - travertine

UR - http://www.scopus.com/inward/record.url?scp=85118705058&partnerID=8YFLogxK

U2 - 10.1134/S1028334X21100081

DO - 10.1134/S1028334X21100081

M3 - Article

AN - SCOPUS:85118705058

VL - 500

SP - 820

EP - 825

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 34615004