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Modern and Paleotravertines from Gorny Altai : Indicative Features. / Kokh, S. N.; Sokol, E. V.; Deev, E. V. и др.

в: Doklady Earth Sciences, Том 483, № 1, 01.12.2018, стр. 1399-1404.

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

Harvard

Kokh, SN, Sokol, EV, Deev, EV, Ryapolova, YM & Rusanov, GG 2018, 'Modern and Paleotravertines from Gorny Altai: Indicative Features', Doklady Earth Sciences, Том. 483, № 1, стр. 1399-1404. https://doi.org/10.1134/S1028334X18110107

APA

Kokh, S. N., Sokol, E. V., Deev, E. V., Ryapolova, Y. M., & Rusanov, G. G. (2018). Modern and Paleotravertines from Gorny Altai: Indicative Features. Doklady Earth Sciences, 483(1), 1399-1404. https://doi.org/10.1134/S1028334X18110107

Vancouver

Kokh SN, Sokol EV, Deev EV, Ryapolova YM, Rusanov GG. Modern and Paleotravertines from Gorny Altai: Indicative Features. Doklady Earth Sciences. 2018 дек. 1;483(1):1399-1404. doi: 10.1134/S1028334X18110107

Author

Kokh, S. N. ; Sokol, E. V. ; Deev, E. V. и др. / Modern and Paleotravertines from Gorny Altai : Indicative Features. в: Doklady Earth Sciences. 2018 ; Том 483, № 1. стр. 1399-1404.

BibTeX

@article{1fcaee3d8b1543bbb0c0eae07c86555c,
title = "Modern and Paleotravertines from Gorny Altai: Indicative Features",
abstract = "Abstract: This work reports new geochemical and stable isotope data on the Late Quaternary travertines of the southeastern Gorny Altai. The travertines are composed of Mg-calcite and Sr-aragonite, which cement the Sartan moraines and Holocene colluvium. The isotope characteristics of CaCO3 (δ13C = –4.1…+0.9‰ and δ18O = –13.8…–13.9‰, VPDB) indicate a mixed carbon source, while the oxygen source is sedimentation water of the early diagenetic stage. The formation of travertines is controlled by the following factors: faults, underlying deformed carbonate rocks, dissected relief overlain by colluvium and/or moraine sediments, and the ascending fluid flow.",
keywords = "TRAVERTINE, ZONE",
author = "Kokh, {S. N.} and Sokol, {E. V.} and Deev, {E. V.} and Ryapolova, {Yu M.} and Rusanov, {G. G.}",
year = "2018",
month = dec,
day = "1",
doi = "10.1134/S1028334X18110107",
language = "English",
volume = "483",
pages = "1399--1404",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "1",

}

RIS

TY - JOUR

T1 - Modern and Paleotravertines from Gorny Altai

T2 - Indicative Features

AU - Kokh, S. N.

AU - Sokol, E. V.

AU - Deev, E. V.

AU - Ryapolova, Yu M.

AU - Rusanov, G. G.

PY - 2018/12/1

Y1 - 2018/12/1

N2 - Abstract: This work reports new geochemical and stable isotope data on the Late Quaternary travertines of the southeastern Gorny Altai. The travertines are composed of Mg-calcite and Sr-aragonite, which cement the Sartan moraines and Holocene colluvium. The isotope characteristics of CaCO3 (δ13C = –4.1…+0.9‰ and δ18O = –13.8…–13.9‰, VPDB) indicate a mixed carbon source, while the oxygen source is sedimentation water of the early diagenetic stage. The formation of travertines is controlled by the following factors: faults, underlying deformed carbonate rocks, dissected relief overlain by colluvium and/or moraine sediments, and the ascending fluid flow.

AB - Abstract: This work reports new geochemical and stable isotope data on the Late Quaternary travertines of the southeastern Gorny Altai. The travertines are composed of Mg-calcite and Sr-aragonite, which cement the Sartan moraines and Holocene colluvium. The isotope characteristics of CaCO3 (δ13C = –4.1…+0.9‰ and δ18O = –13.8…–13.9‰, VPDB) indicate a mixed carbon source, while the oxygen source is sedimentation water of the early diagenetic stage. The formation of travertines is controlled by the following factors: faults, underlying deformed carbonate rocks, dissected relief overlain by colluvium and/or moraine sediments, and the ascending fluid flow.

KW - TRAVERTINE

KW - ZONE

UR - http://www.scopus.com/inward/record.url?scp=85058852394&partnerID=8YFLogxK

U2 - 10.1134/S1028334X18110107

DO - 10.1134/S1028334X18110107

M3 - Article

AN - SCOPUS:85058852394

VL - 483

SP - 1399

EP - 1404

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 17927366