Low-pH waters discharging from submarine vents at Panarea Island (Aeolian Islands, southern Italy) after the 2002 gas blast: Origin of hydrothermal fluids and implications for volcanic surveillance

Autor: Tassi F.[1], Capaccioni B.[2], Caramanna G.[3], Cinti D.[3], Montegrossi G.[4], Pizzino L.[3], Quattrocchi F.[3], Vaselli O.[1

Publikováno v: Applied geochemistry 24 (2009): 246–254. doi:10.1016/j.apgeochem.2008.11.015
info:cnr-pdr/source/autori:Tassi F.[1], Capaccioni B.[2], Caramanna G.[3], Cinti D.[3], Montegrossi G.[4], Pizzino L.[3], Quattrocchi F.[3], Vaselli O.[1,4]/titolo:Low-pH waters discharging from submarine vents at Panarea Island (Aeolian islands, southern Italy) after the 2002 gas blast: Origin of hydrothermal fluids and implications for volcanic surveillance/doi:10.1016%2Fj.apgeochem.2008.11.015/rivista:Applied geochemistry/anno:2009/pagina_da:246/pagina_a:254/intervallo_pagine:246–254/volume:24

A geochemical survey of thermal waters collected from submarine vents at Panarea Island (Aeolian islands, southern Italy) was carried out from December 2002 to March 2007, in order to investigate (i) the geochemical processes controlling the chemical

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e70dd461b0fb737da80ed1cefbad47ad
https://doi.org/10.1016/j.apgeochem.2008.11.015