Temporal evolution of flow conditions in sustained magmatic explosive eruptions

Journal of Volcanology and Geothermal Research

Volumn 143, Issue 1-3, 2005, Pages 153-172

  Macedonio, G ^a   Neri, A ^b   Marti J ^c   Folch, A ^c  

^a OSSERVATORIO VESUVIANO   (Italy)

^b SEZIONE DI PISA   (Italy)

^c INSTITUTE OF EARTH SCIENCES JAUME ALMERA   (Spain)

Author keywords

Conduit flow; Explosive eruptions; Magma chamber discharge; Pressure evolution; Temporal evolution

Indexed keywords

COMPUTER SIMULATION; CONFINED FLOW; EXPLOSIVES; HYDROSTATIC PRESSURE; ISOTHERMS; MASS TRANSFER; MATHEMATICAL MODELS; NUCLEATION; SHEAR STRESS; THERMAL STRATIFICATION;

FLOW PRESSURE; MAGMATIC EXPLOSIVE ERUPTIONS; MASS FLOW-RATE; MASS FRACTIONS;

VOLCANOES;

EXPLOSIVE VOLCANISM; LAVA FLOW; NUMERICAL MODEL; PRESSURE GRADIENT; TEMPORAL EVOLUTION;

EID: 19944397888     PISSN: 03770273     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jvolgeores.2004.09.015     Document Type: Article

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