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pro vyhledávání: '"Pruiti L. (3)"'
Publikováno v:
11th Water-Rock Interaction (WRI-11), pp. 95–99, Saratoga Springs (NY), USA, June 2004
info:cnr-pdr/source/autori:Carapezza M.L. (1); Cioni R. (2); Guidi M. (2); Scozzari A. (2); Pruiti L. (3)/congresso_nome:11th Water-Rock Interaction (WRI-11)/congresso_luogo:Saratoga Springs (NY), USA/congresso_data:June 2004/anno:2004/pagina_da:95/pagina_a:99/intervallo_pagine:95–99
info:cnr-pdr/source/autori:Carapezza M.L. (1); Cioni R. (2); Guidi M. (2); Scozzari A. (2); Pruiti L. (3)/congresso_nome:11th Water-Rock Interaction (WRI-11)/congresso_luogo:Saratoga Springs (NY), USA/congresso_data:June 2004/anno:2004/pagina_da:95/pagina_a:99/intervallo_pagine:95–99
Chemical-physical modifications of groundwater in active volcanic areas provide important insights on magma ascent leading to volcanic eruptions. To fully exploit the great potential of fluid geochemistry, the traditional discontinuous sampling with
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::321c3dabbfed5b61917f9d25ca293a8f
http://www.cnr.it/prodotto/i/83375
http://www.cnr.it/prodotto/i/83375