Equilibrium of nitrogen-rich spring waters of the Baikal Rift Zone with host rock minerals as a basis for determining mechanisms of their formation

Author:

Shvartsev S. L.,Zamana L. V.,Plyusnin A. M.,Tokarenko O. G.

Publisher

Pleiades Publishing Ltd

Subject

Geochemistry and Petrology,Geophysics

Reference58 articles.

1. V. A. Alekseev, B. N. Ryzhenko, S. L. Shvartsev, V. P. Zverev, V. P. Bukaty, M. V. Mironenko, M. V. Charykova, and O. V. Chudaev, Geological Evolution and SelfOrganization of the Water–Rock System. Vol. 1 Water–Rock System in the Earth’s Crust: Interaction, Kinetics, Equilibrium, and Modeling (Sib. Otd. Ross. Akad. Nauk., Novosibirsk, 2005) [in Russian].

2. D. M. Allen, S. E. Graspy, and D. A. Voormeij, “Determining the circulation depth of thermal spring in the southern Rocky Mountain Trench, southeastern British Columbia, Canada using geochemistry and borehole temperature logs,” Hydrogeol. J. 14 (1–2), 159–172 (2006).

3. L. N. Barabanov and V. N. Disler, Nitric Thermal Waters of the USSR (TsNIIKF, Moscow, 1968) [in Russian].

4. H. L. Barnes, “Solubility of ore minerals,” in Geochemistry of Hydrothermal Ore Deposits, Ed. by H.L. Barnes (Wiley, New York, 1982).

5. E. A. Baskov and G. I. Klimov, “Composition and conditions of formation of Transbaikalian waters” Tr. Vses. Nauch.Issled. Geol. Inst. Nov. Ser. 101, 50–88 (1963).

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