Effect of syneruptive decompression path on shifting intensity in basaltic sub-Plinian eruption: Implication of microlites in Yufune-2 scoria from Fuji volcano, Japan

Journal of Volcanology and Geothermal Research

Volumn 198, Issue 1-2, 2010, Pages 158-176

  Suzuki, Yuki ^a   Fujii, Toshitsugu ^a  

^a UNIVERSITY OF TOKYO   (Japan)

Author keywords

Basaltic Plinian; Conduit flow; Crystal size distribution; Microlite; Outgassing

Indexed keywords

CONDUIT FLOW; CRYSTAL SIZE DISTRIBUTION; MICROLITES; OUTGASSING; PLINIAN;

CONFINED FLOW; DEGASSING; GRAIN SIZE AND SHAPE; PETROGRAPHY; PHASE SEPARATION; SIZE DETERMINATION; SIZE DISTRIBUTION; VOLCANOES;

BASALT;

CRYSTALLIZATION; DECOMPRESSION; FLOW VELOCITY; LAVA; LITHIC FRAGMENT; MAGMA CHAMBER; PETROGRAPHY; PLINIAN ERUPTION; SIZE DISTRIBUTION; TEMPORAL VARIATION; VOLCANIC ERUPTION;

CHUBU; FUJI; HONSHU; JAPAN; SHIZUOKA [CHUBU];

PLINIA;

EID: 78650075593     PISSN: 03770273     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jvolgeores.2010.08.020     Document Type: Article

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