Инд. авторы:	Kokh S.N., Sokol E.V., Deev E.V., Ryapolova Y.M., Rusanov G.G.
Заглавие:	Modern and Paleotravertines from Gorny Altai: Indicative Features
Библ. ссылка:	Kokh S.N., Sokol E.V., Deev E.V., Ryapolova Y.M., Rusanov G.G. Modern and Paleotravertines from Gorny Altai: Indicative Features // Doklady Earth Sciences. - 2018. - Vol.483. - Iss. 1. - P.1399-1404. - ISSN 1028-334X. - EISSN 1531-8354.
Внешние системы:	DOI: 10.1134/S1028334X18110107; SCOPUS: 2-s2.0-85058852394; WoS: 000453745300006;
Реферат:	eng: 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 (C-13 = -4.1...+0.9 parts per thousand and O-18 = -13.8...-13.9 parts per thousand, 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.
Ключевые слова:	ZONE; TRAVERTINE;
Издано:	2018
Физ. характеристика:	с.1399-1404