Modern and Paleotravertines from Gorny Altai: Indicative Features


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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 CaCO313C = –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.

About the authors

S. N. Kokh

V.S. Sobolev Institute of Geology and Mineralogy,
Siberian Branch, Russian Academy of Sciences

Author for correspondence.
Email: s.n.kokh@gmail.com
Russian Federation, Novosibirsk, 630090

E. V. Sokol

V.S. Sobolev Institute of Geology and Mineralogy,
Siberian Branch, Russian Academy of Sciences

Email: s.n.kokh@gmail.com
Russian Federation, Novosibirsk, 630090

E. V. Deev

Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Sciences; Novosibirsk State University

Email: s.n.kokh@gmail.com
Russian Federation, Novosibirsk, 630090; Novosibirsk, 630090

Yu. M. Ryapolova

Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Sciences

Email: s.n.kokh@gmail.com
Russian Federation, Novosibirsk, 630090

G. G. Rusanov

JSC Gorno-Altaiskaya Expedition

Email: s.n.kokh@gmail.com
Russian Federation, Maloyeniseiskoe, Altaiskii krai


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