Abstract
The study area is the South Tatarstan Arch located in the Volgo-Ural Region, which is an enigmatic crustal segment occupying one third of the East European Platform. Monitoring studies have shown that fluid discharge processes are still active and time-dependent. This paper presents an integrated review of the geological, geophysical, hydrochemical and geochemical studies of the crystalline basement of Tatarstan. These studies are based on the stratigraphic and compositional schemes within the crystalline basement, the drilling of deep wells, the geodynamic activity of the fractured zones of the crystalline basement and the presence of fluids therein. Furthermore, the changes in the chemical composition of the basement waters are taken into account.
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Acknowledgments
The author expresses her profound gratitude to Prof. Renat Kh. Muslimov for his long-term guidance of the crystalline basement studies, the results of which have formed the core of this work, and to Prof. Alexander V. Postnikov, Prof. Danis K. Nurgaliev and Prof. Natalya N. Khristoforova for discussing these materials and for the valuable comments and generous help in preparing this paper. The author thanks Prof. Rimma P. Gottikh, and Prof. Bogdan I.Pisotsky for suggestions that improved the manuscript and for the useful discussions and support.
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Plotnikova, I.N. New data on the present-day active fluid regime of fractured zones of crystalline basement and sedimentary cover in the eastern part of Volga-Ural region. Int J Earth Sci (Geol Rundsch) 97, 1131–1142 (2008). https://doi.org/10.1007/s00531-007-0274-z
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DOI: https://doi.org/10.1007/s00531-007-0274-z