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Dulinski M.,AGH University of Science and Technology | Rajchel L.,AGH Akademia Gomiczo Hutnicza | Czop M.,AGH University of Science and Technology | Motyka J.,AGH University of Science and Technology | Rajchel J.,AGH University of Science and Technology
Biuletyn - Panstwowego Instytutu Geologicznego | Year: 2013

The mineral waters of the Iwonicz and Rymanów areas are characterised by increased mineralisation, typically in the order of dozens g/dm3, with a significant contribution from the chloride component. Their stable isotope composition differs from the Global Meteoric Water Line (GM WL) indicating that all investigated waters represent a mixture of both young infiltration and diagenetic waters of deep circulation. Obtained results point to significant participation of young infiltration components in analysed waters whose age is between 10-20 years old. Source

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