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Late Pleistocene-Holocene coseismic deformations in the Malyi Yaloman River Valley (Gorny Altai). / Deev, E. V.; Zolnikov, I. D.; Lobova, E. Yu.

In: Russian Geology and Geophysics, Vol. 56, No. 9, 01.09.2015, p. 1256-1272.

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

Harvard

Deev, EV, Zolnikov, ID & Lobova, EY 2015, 'Late Pleistocene-Holocene coseismic deformations in the Malyi Yaloman River Valley (Gorny Altai)', Russian Geology and Geophysics, vol. 56, no. 9, pp. 1256-1272. https://doi.org/10.1016/j.rgg.2015.08.003

APA

Deev, E. V., Zolnikov, I. D., & Lobova, E. Y. (2015). Late Pleistocene-Holocene coseismic deformations in the Malyi Yaloman River Valley (Gorny Altai). Russian Geology and Geophysics, 56(9), 1256-1272. https://doi.org/10.1016/j.rgg.2015.08.003

Vancouver

Deev EV, Zolnikov ID, Lobova EY. Late Pleistocene-Holocene coseismic deformations in the Malyi Yaloman River Valley (Gorny Altai). Russian Geology and Geophysics. 2015 Sept 1;56(9):1256-1272. doi: 10.1016/j.rgg.2015.08.003

Author

Deev, E. V. ; Zolnikov, I. D. ; Lobova, E. Yu. / Late Pleistocene-Holocene coseismic deformations in the Malyi Yaloman River Valley (Gorny Altai). In: Russian Geology and Geophysics. 2015 ; Vol. 56, No. 9. pp. 1256-1272.

BibTeX

@article{79bd7e4533224fcb969ee0d7c66c213b,
title = "Late Pleistocene-Holocene coseismic deformations in the Malyi Yaloman River Valley (Gorny Altai)",
abstract = "Palaeoseismological studies were performed within the Yaloman graben (Gorny Altai). Five Quaternary sections with coseismic deformation structures (seismites) have been recognized in the lower course of the Malyi Yaloman River. Traces of ancient earthquakes are localized at two levels (Late Pleistocene-Holocene). The most likely mechanisms of the seismite formation are brittle failure, liquefaction, and fluidization. The types of coseismic deformations and their sizes suggest that the Yaloman graben was the locus of prehistoric earthquakes with M > 5-7, although modern-day seismic activity consists of smaller-magnitude earthquakes. This should be taken into account in assessing the seismic hazards during construction of gas pipeline to China and tourism infrastructure facilities.",
keywords = "Earthquakes, Gorny altai, Quaternary deposits, Seismites, Yaloman graben",
author = "Deev, {E. V.} and Zolnikov, {I. D.} and Lobova, {E. Yu}",
year = "2015",
month = sep,
day = "1",
doi = "10.1016/j.rgg.2015.08.003",
language = "English",
volume = "56",
pages = "1256--1272",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "9",

}

RIS

TY - JOUR

T1 - Late Pleistocene-Holocene coseismic deformations in the Malyi Yaloman River Valley (Gorny Altai)

AU - Deev, E. V.

AU - Zolnikov, I. D.

AU - Lobova, E. Yu

PY - 2015/9/1

Y1 - 2015/9/1

N2 - Palaeoseismological studies were performed within the Yaloman graben (Gorny Altai). Five Quaternary sections with coseismic deformation structures (seismites) have been recognized in the lower course of the Malyi Yaloman River. Traces of ancient earthquakes are localized at two levels (Late Pleistocene-Holocene). The most likely mechanisms of the seismite formation are brittle failure, liquefaction, and fluidization. The types of coseismic deformations and their sizes suggest that the Yaloman graben was the locus of prehistoric earthquakes with M > 5-7, although modern-day seismic activity consists of smaller-magnitude earthquakes. This should be taken into account in assessing the seismic hazards during construction of gas pipeline to China and tourism infrastructure facilities.

AB - Palaeoseismological studies were performed within the Yaloman graben (Gorny Altai). Five Quaternary sections with coseismic deformation structures (seismites) have been recognized in the lower course of the Malyi Yaloman River. Traces of ancient earthquakes are localized at two levels (Late Pleistocene-Holocene). The most likely mechanisms of the seismite formation are brittle failure, liquefaction, and fluidization. The types of coseismic deformations and their sizes suggest that the Yaloman graben was the locus of prehistoric earthquakes with M > 5-7, although modern-day seismic activity consists of smaller-magnitude earthquakes. This should be taken into account in assessing the seismic hazards during construction of gas pipeline to China and tourism infrastructure facilities.

KW - Earthquakes

KW - Gorny altai

KW - Quaternary deposits

KW - Seismites

KW - Yaloman graben

UR - http://www.scopus.com/inward/record.url?scp=84939611642&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2015.08.003

DO - 10.1016/j.rgg.2015.08.003

M3 - Article

AN - SCOPUS:84939611642

VL - 56

SP - 1256

EP - 1272

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 9

ER -

ID: 25488204