A CO2-rich gas trigger of explosive paroxysms at Stromboli basaltic volcano, Italy

Journal of Volcanology and Geothermal Research

Volumn 189, Issue 3-4, 2010, Pages 363-374

  Allard, Patrick ^a,b  

^a CNRS   (France)

^b ISTITUTO NAZIONALE DI GEOFISICA E VULCANOLOGIA   (Italy)

Author keywords

basaltic volcanoes; CO2; explosive paroxysms; gas bubbles; magma degassing

Indexed keywords

BASALTIC MAGMA; BASALTIC VOLCANOES; CLOSED SYSTEMS; DRIVING FORCES; FOAM COLLAPSE; FOAM GROWTH; GAS BUBBLE; GAS BUBBLES; GAS COMPOSITIONS; GAS POCKETS; GAS PRESSURES; GASPHASE; GREAT DEPTH; LOW VISCOSITY; MAGMA BLOBS; MAGMA DEGASSING; MAJOR HAZARDS; MOLAR RATIO; PLUMBING SYSTEMS; STROMBOLI VOLCANO; STROMBOLIAN ACTIVITY; TIME-AVERAGED; VESICULARITY;

BASALT; CARBON DIOXIDE; CARBON MONOXIDE; DEGASSING; EXPLOSIVES; FEEDING; GASES; METALLIC GLASS; PLUMBING; SURFACE CHEMISTRY; VOLCANOES;

PHASE INTERFACES;

AIR BUBBLE; BASALT; CARBON DIOXIDE; CRATER; CRYSTALLIZATION; DECOMPRESSION; DEGASSING; EXPLOSIVE VOLCANISM; HYDROTHERMAL PLUME; MAGMATISM; NUMERICAL MODEL; PUMICE; VISCOSITY; VOLCANIC GAS; VOLCANOLOGY;

ITALY; LIPARI ISLANDS; MESSINA [SICILY]; SICILY; STROMBOLI;

EID: 73849146077     PISSN: 03770273     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jvolgeores.2009.11.018     Document Type: Article

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