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Paleoearthquakes in the Uimon basin (Gorny Altai). / Deev, E. V.; Zol'nikov, I. D.; Turova, I. V. et al.

In: Russian Geology and Geophysics, Vol. 59, No. 4, 01.04.2018, p. 351-362.

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

Harvard

Deev, EV, Zol'nikov, ID, Turova, IV, Rusanov, GG, Ryapolova, YM, Nevedrova, NN & Kotler, SA 2018, 'Paleoearthquakes in the Uimon basin (Gorny Altai)', Russian Geology and Geophysics, vol. 59, no. 4, pp. 351-362. https://doi.org/10.1016/j.rgg.2017.07.011

APA

Deev, E. V., Zol'nikov, I. D., Turova, I. V., Rusanov, G. G., Ryapolova, Y. M., Nevedrova, N. N., & Kotler, S. A. (2018). Paleoearthquakes in the Uimon basin (Gorny Altai). Russian Geology and Geophysics, 59(4), 351-362. https://doi.org/10.1016/j.rgg.2017.07.011

Vancouver

Deev EV, Zol'nikov ID, Turova IV, Rusanov GG, Ryapolova YM, Nevedrova NN et al. Paleoearthquakes in the Uimon basin (Gorny Altai). Russian Geology and Geophysics. 2018 Apr 1;59(4):351-362. doi: 10.1016/j.rgg.2017.07.011

Author

Deev, E. V. ; Zol'nikov, I. D. ; Turova, I. V. et al. / Paleoearthquakes in the Uimon basin (Gorny Altai). In: Russian Geology and Geophysics. 2018 ; Vol. 59, No. 4. pp. 351-362.

BibTeX

@article{67efaaba9e7a4d96a3b7745e40e8aa6b,
title = "Paleoearthquakes in the Uimon basin (Gorny Altai)",
abstract = "Paleoseismological studies confirm that the Uimon basin is thrust by its northern mountain border along the active South Terekta fault. The latest motion along the fault in the 7-8th centuries AD induced an earthquake with a magnitude of Mw= 7.4-7.7 and a shaking intensity of I = 9-11 on the MSK-64 scale. The same fault generated another event (M > 7, I = 9-10), possibly, about 16 kyr ago, which triggered gravity sliding. The rockslide dammed the Uimon valley and produced a lake, where lacustrine deposition began about 14 ± 1 kyr ago, and a later M > 7 (I = 9-10) earthquake at ~ 6 ka caused the dam collapse and the lake drainage. Traces of much older earthquakes that occurred within the Uimon basin are detectable from secondary deformation structures (seismites) in soft sediments deposited during the drainage of a Late Pleistocene ice-dammed lake between 100 and 90 ka and in ~ 77 ka alluvium. The magnitude and intensity of these paleoearthquakes were at least M > 5.0-5.5 and I > 6-7.",
keywords = "Gorny Altai, large paleoearthquakes, paleoseismology, primary and secondary seismic deformations, Uimon basin, DEPRESSION, SEDIMENTS, ZONE, EMPIRICAL RELATIONSHIPS, DEFORMATION, MAGNITUDE, ANCIENT EARTHQUAKES, DEPOSITS, MONGOLIA, KINEMATICS",
author = "Deev, {E. V.} and Zol'nikov, {I. D.} and Turova, {I. V.} and Rusanov, {G. G.} and Ryapolova, {Yu M.} and Nevedrova, {N. N.} and Kotler, {S. A.}",
year = "2018",
month = apr,
day = "1",
doi = "10.1016/j.rgg.2017.07.011",
language = "English",
volume = "59",
pages = "351--362",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "4",

}

RIS

TY - JOUR

T1 - Paleoearthquakes in the Uimon basin (Gorny Altai)

AU - Deev, E. V.

AU - Zol'nikov, I. D.

AU - Turova, I. V.

AU - Rusanov, G. G.

AU - Ryapolova, Yu M.

AU - Nevedrova, N. N.

AU - Kotler, S. A.

PY - 2018/4/1

Y1 - 2018/4/1

N2 - Paleoseismological studies confirm that the Uimon basin is thrust by its northern mountain border along the active South Terekta fault. The latest motion along the fault in the 7-8th centuries AD induced an earthquake with a magnitude of Mw= 7.4-7.7 and a shaking intensity of I = 9-11 on the MSK-64 scale. The same fault generated another event (M > 7, I = 9-10), possibly, about 16 kyr ago, which triggered gravity sliding. The rockslide dammed the Uimon valley and produced a lake, where lacustrine deposition began about 14 ± 1 kyr ago, and a later M > 7 (I = 9-10) earthquake at ~ 6 ka caused the dam collapse and the lake drainage. Traces of much older earthquakes that occurred within the Uimon basin are detectable from secondary deformation structures (seismites) in soft sediments deposited during the drainage of a Late Pleistocene ice-dammed lake between 100 and 90 ka and in ~ 77 ka alluvium. The magnitude and intensity of these paleoearthquakes were at least M > 5.0-5.5 and I > 6-7.

AB - Paleoseismological studies confirm that the Uimon basin is thrust by its northern mountain border along the active South Terekta fault. The latest motion along the fault in the 7-8th centuries AD induced an earthquake with a magnitude of Mw= 7.4-7.7 and a shaking intensity of I = 9-11 on the MSK-64 scale. The same fault generated another event (M > 7, I = 9-10), possibly, about 16 kyr ago, which triggered gravity sliding. The rockslide dammed the Uimon valley and produced a lake, where lacustrine deposition began about 14 ± 1 kyr ago, and a later M > 7 (I = 9-10) earthquake at ~ 6 ka caused the dam collapse and the lake drainage. Traces of much older earthquakes that occurred within the Uimon basin are detectable from secondary deformation structures (seismites) in soft sediments deposited during the drainage of a Late Pleistocene ice-dammed lake between 100 and 90 ka and in ~ 77 ka alluvium. The magnitude and intensity of these paleoearthquakes were at least M > 5.0-5.5 and I > 6-7.

KW - Gorny Altai

KW - large paleoearthquakes

KW - paleoseismology

KW - primary and secondary seismic deformations

KW - Uimon basin

KW - DEPRESSION

KW - SEDIMENTS

KW - ZONE

KW - EMPIRICAL RELATIONSHIPS

KW - DEFORMATION

KW - MAGNITUDE

KW - ANCIENT EARTHQUAKES

KW - DEPOSITS

KW - MONGOLIA

KW - KINEMATICS

UR - http://www.scopus.com/inward/record.url?scp=85045240723&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2017.07.011

DO - 10.1016/j.rgg.2017.07.011

M3 - Article

AN - SCOPUS:85045240723

VL - 59

SP - 351

EP - 362

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 4

ER -

ID: 12542950