Geohemijski značaj serpentinita u formiranju sastava termalne vode Gorje Trepče (okolina Čačka, Srbija)

Geochemical importance of serpentinites influencing composition of Gornja Trepča thermal water near Čačak (Serbia)

  • Damnjan Protić Geoinstitute, Rovinjska 12, 11000 Belgrade, Serbia.
  • Vojislav Tomić University of Belgrade, Faculty of Mining and Geology, Đušina 7, 11000 Belgrade, Serbia.
  • Sladjan Timotijević Geoinstitute, Rovinjska 12, 11000 Belgrade, Serbia.
Keywords: thermal water, magnesium, geochemistry serpentinites, hydrolysis of silicates, Gonja Trepča, Čačak, Serbia

Abstract

The Gonja Trepča thermal water with increased Mg2+ is of HCO3-Mg2Ca type. The problem of origin of Mg2+ in water has been solved in this work by use of geochemical thermodynamical calculations of the water-rock interaction. The calculation shows that water has been enriched in magnesium by filtration trough serpentinites or that serpentinites represent the roof barrier of the Gomja Trepca hydrogeological structure respectively. It is necessary this roof barrier to be drilled in aim the warmer thermal water to be captured.

 

Published
1998-12-19
How to Cite
Protić, D., Tomić, V. and Timotijević, S. (1998) “Geohemijski značaj serpentinita u formiranju sastava termalne vode Gorje Trepče (okolina Čačka, Srbija)”, Geološki anali Balkanskoga poluostrva, 62(1), pp. 367-374. Available at: https://gabp.rgf.bg.ac.rs/index.php/gabp/article/view/362 (Accessed: 22December2024).
Issue
Vol 62 No 1 (1998): Geološki anali Balkanskoga poluostrva
Section
Original Scientific Paper

Copyright (c) 1998 Geološki anali Balkanskoga poluostrva

Creative Commons License

This work is licensed under a Creative Commons Attribution 4.0 International License.