A fragmentation criterion for highly viscous bubbly magmas estimated from shock tube experiments

Journal of Volcanology and Geothermal Research

Volumn 178, Issue 1, 2008, Pages 58-71

  Koyaguchi, Takehiro ^a   Scheu, Bettina ^a   Mitani, Noriko K ^a   Melnik, Oleg ^b  

^a UNIVERSITY OF TOKYO   (Japan)

^b MOSCOW STATE UNIVERSITY   (Russian Federation)

Author keywords

explosive volcanic eruptions; magma fragmentation criterion; shock tube experiments; shock tube theory

Indexed keywords

EXPERIMENTS; POROSITY; SHOCK TUBES; TUBES (COMPONENTS); VOLCANIC ROCKS; VOLCANOES;

BUBBLE WALLS; CRITICAL VALUES; DOMINANT FACTORS; EXPERIMENTAL DATUMS; GEOPHYSICAL RESEARCHES; INITIAL PRESSURES; LAYER BY LAYERS; MAGMA FRAGMENTATION CRITERION; OVER PRESSURES; PRESSURE INCREASES; SHOCK TUBE THEORY; SQUARE ROOTS; THEORETICAL MODELS; TUBE THEORIES;

SHOCK WAVES;

FRAGMENTATION; MAGMA; MICROCRACK; OVERPRESSURE; POROSITY; TENSILE STRESS; VISCOSITY; VOLCANIC ERUPTION;

EID: 55549139480     PISSN: 03770273     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jvolgeores.2008.02.008     Document Type: Article

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