Том: Procedia Earth and Planetary Science: Proceedings of the Fourteenth International Symposium on Water-Rock Interaction, WRI 14 (Palais des Papes, Avignon, France, 9-14 June 2013)
Том: 7
, Год издания: 2013
Многотомное издание: Procedia Earth and Planetary Science: Proceedings of the Fourteenth International Symposium on Water-Rock Interaction, WRI 14 (Palais des Papes, Avignon, France, 9-14 June 2013)
Страницы: 444-447
Аннотация
This article presents data on the chemical composition of soda lakes in western Mongolia, describes and graphically represents the equilibrium of the water with carbonate, sulfate, and aluminosilicate minerals. We conclude that the soda lakes are products of water-rock interaction that resulted in precipitation of carbonate minerals under conditions of high water exchange and arid climate, and has lasted a geologically long time. (C) 2012 The Authors. Published by Elsevier B.V.
