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Comparative analysis of megaflood deposits and alluvium of the Chuya and Katun' river valleys (Gorny Altai). / Zolnikov, I.D.; Deev, E.V.; Nazarov, D.V.; Kotler, S.A.

в: Russian Geology and Geophysics, № 8, 2015, стр. 1162-1172.

Результаты исследований: Научные публикации в периодических изданиях › статья

Harvard

Zolnikov, ID, Deev, EV, Nazarov, DV & Kotler, SA 2015, 'Comparative analysis of megaflood deposits and alluvium of the Chuya and Katun' river valleys (Gorny Altai)', Russian Geology and Geophysics, № 8, стр. 1162-1172. https://doi.org/10.1016/j.rgg.2015.07.007

APA

Zolnikov, I. D., Deev, E. V., Nazarov, D. V., & Kotler, S. A. (2015). Comparative analysis of megaflood deposits and alluvium of the Chuya and Katun' river valleys (Gorny Altai). Russian Geology and Geophysics, (8), 1162-1172. https://doi.org/10.1016/j.rgg.2015.07.007

Vancouver

Zolnikov ID, Deev EV, Nazarov DV, Kotler SA. Comparative analysis of megaflood deposits and alluvium of the Chuya and Katun' river valleys (Gorny Altai). Russian Geology and Geophysics. 2015;(8):1162-1172. https://doi.org/10.1016/j.rgg.2015.07.007

Author

Zolnikov, I.D. ; Deev, E.V. ; Nazarov, D.V. ; Kotler, S.A. / Comparative analysis of megaflood deposits and alluvium of the Chuya and Katun' river valleys (Gorny Altai). в: Russian Geology and Geophysics. 2015 ; № 8. стр. 1162-1172.

BibTeX

@article{3797d742d7564e91868afc7a4660ed9e,
title = "Comparative analysis of megaflood deposits and alluvium of the Chuya and Katun' river valleys (Gorny Altai)",
abstract = "{\textcopyright} 2015.Sedimentary indicators of catastrophic glacial megafloods-plane-bedded angular gravel, cobbles, and boulders-are described in several sections of the high terraces of the Chuya River valley. The principal difference of these sediments from typical alluvium of this area is demonstrated. The clast roundness, grain size of clasts, and sedimentary structures of the high-terrace deposits of the Chuya and Katun' valleys indicate the same facies originated through megaflood deposition. These results are at odds with ideas of alluvial, glacial, or glaciofluvial genesis of the high-terrace deposits of the Chuya River.",
author = "I.D. Zolnikov and E.V. Deev and D.V. Nazarov and S.A. Kotler",
year = "2015",
doi = "10.1016/j.rgg.2015.07.007",
language = "English",
pages = "1162--1172",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier",
number = "8",

}

RIS

TY - JOUR

T1 - Comparative analysis of megaflood deposits and alluvium of the Chuya and Katun' river valleys (Gorny Altai)

AU - Zolnikov, I.D.

AU - Deev, E.V.

AU - Nazarov, D.V.

AU - Kotler, S.A.

PY - 2015

Y1 - 2015

N2 - © 2015.Sedimentary indicators of catastrophic glacial megafloods-plane-bedded angular gravel, cobbles, and boulders-are described in several sections of the high terraces of the Chuya River valley. The principal difference of these sediments from typical alluvium of this area is demonstrated. The clast roundness, grain size of clasts, and sedimentary structures of the high-terrace deposits of the Chuya and Katun' valleys indicate the same facies originated through megaflood deposition. These results are at odds with ideas of alluvial, glacial, or glaciofluvial genesis of the high-terrace deposits of the Chuya River.

AB - © 2015.Sedimentary indicators of catastrophic glacial megafloods-plane-bedded angular gravel, cobbles, and boulders-are described in several sections of the high terraces of the Chuya River valley. The principal difference of these sediments from typical alluvium of this area is demonstrated. The clast roundness, grain size of clasts, and sedimentary structures of the high-terrace deposits of the Chuya and Katun' valleys indicate the same facies originated through megaflood deposition. These results are at odds with ideas of alluvial, glacial, or glaciofluvial genesis of the high-terrace deposits of the Chuya River.

U2 - 10.1016/j.rgg.2015.07.007

DO - 10.1016/j.rgg.2015.07.007

M3 - Article

SP - 1162

EP - 1172

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 8

ER -

ID: 4011475