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

Applied Geochemistry

Volumn 24, Issue 2, 2009, Pages 246-254

  Tassi, Franco ^a   Capaccioni, Bruno ^b   Caramanna, Giorgio ^c   Cinti, Daniele ^c   Montegrossi, Giordano ^d   Pizzino, Luca ^c   Quattrocchi, Fedora ^c   Vaselli, Orlando ^a,d  

^a UNIVERSITY OF FLORENCE   (Italy)

^b UNIVERSITY OF BOLOGNA   (Italy)

^c ISTITUTO NAZIONALE DI GEOFISICA E VULCANOLOGIA   (Italy)

^d SEZIONE DI FIRENZE   (Italy)

Author keywords

[No Author keywords available]

Indexed keywords

APPROXIMATION THEORY; CALCIUM; MINERALS; SALINE WATER; SEAWATER; SODIUM; SUBMARINES; VENTS;

AEOLIAN ISLANDS; CHEMICAL COMPOSITIONS; CHEMICAL FEATURES; COMPOSITIONAL DATUMS; CONCEPTUAL MODELS; EQUILIBRIUM TEMPERATURES; GEOCHEMICAL PROCESSES; GEOCHEMICAL SURVEYS; GEOTHERMOMETER; GEOTHERMOMETRY; HIGH TEMPERATURES; HYDROTHERMAL FLUIDS; MAGMATIC SYSTEMS; ROCK INTERACTIONS; THERMAL WATERS; VOLCANIC SURVEILLANCES; WATER SAMPLES;

WATER CONTENT;

CHEMICAL COMPOSITION; DISCHARGE; GEOCHEMICAL SURVEY; HYDROTHERMAL FLUID; HYDROTHERMAL VENT; PH; RESERVOIR; THERMAL WATER; UNDERWATER ENVIRONMENT;

EURASIA; EUROPE; ITALY; LIPARI ISLANDS; MESSINA [SICILY]; PANAREA; SICILY; SOUTHERN EUROPE;

EID: 58349111177     PISSN: 08832927     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.apgeochem.2008.11.015     Document Type: Article

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