Mixing processes and water-rock interaction in contrasting geologic environments of Mexico and Hungary Conference Paper uri icon

abstract

  • Ahydrochemical comparison between a carbonate (Mexico) and a non-carbonate (Hungary) system is presented. Major and trace elements, δ 2H and δ 18Ovalues were studied. Although the geological conditions and the concentration of the major elements were different, common features and/or processes were recognized. The main similarity was the distribution of the stable isotope δ values (meteoric and non-meteoric water), and the behavior of As and Mo oxy-anions. Mixing with highly saline water of sea origin is an important process in both areas. © 2010 Taylor %26amp; Francis Group, London.

publication date

  • 2010-01-01