A geochemical traverse across the eastern Carpathians (Romania): Constraints on the origin and evolution of the mineral water and gas discharges

Autor: Vaselli O. (1, Minissale A. (2), Tassi F. (1), Magro G. (3), Seghedi I. (4), Ioane D.(4), Szakacs A. (4)

Publikováno v: Chemical geology 182 (2002): 637–654. doi:10.1016/S0009-2541(01)00348-5
info:cnr-pdr/source/autori:Vaselli O. (1,2), Minissale A. (2), Tassi F. (1), Magro G. (3), Seghedi I. (4), Ioane D.(4), Szakacs A. (4)/titolo:A geochemical traverse across the eastern Carpathians (Romania): Constraints on the origin and evolution of the mineral water and gas discharges./doi:10.1016%2FS0009-2541(01)00348-5/rivista:Chemical geology/anno:2002/pagina_da:637/pagina_a:654/intervallo_pagine:637–654/volume:182

The inner sector of the Eastern Carpathians displays a large number of Na–HCO 3 , CO 2 -rich, meteoric-originated cold springs (soda springs) and bore wells, as well as dry mofettes. They border the southern part of the Pliocene–Quaternary Calima

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d26b33a1b89fea05e50390a1e24015c5
https://publications.cnr.it/doc/29124