H2O-rich melt inclusions in fayalitic olivine from Hekla volcano: Implications for phase relationships in silicic systems and driving forces of explosive volcanism on Iceland

Earth and Planetary Science Letters

Volumn 357-358, Issue , 2012, Pages 337-346

  Portnyagin, Maxim ^a,b   Hoernle, Kaj ^a   Storm, Sonja ^c   Mironov, Nikita ^b   van den Bogaard, Christel ^a   Botcharnikov, Roman ^d  

^a GEOMAR HELMHOLTZ CENTRE FOR OCEAN RESEARCH KIEL   (Germany)

^b VERNADSKY INSTITUTE OF GEOCHEMISTRY AND ANALYTICAL CHEMISTRY   (Russian Federation)

^c UNIVERSITY OF AUCKLAND   (New Zealand)

^d LEIBNIZ UNIVERSITY HANNOVER   (Germany)

Author keywords

Explosive volcanism; H2O; Melt inclusions; Olivine; Oxygen fugacity; Volatiles

Indexed keywords

ANHYDROUS MINERALS; CRYSTAL FRACTIONATION; DRIVING FORCES; ENDMEMBERS; EXPLOSIVE ERUPTION; EXPLOSIVE VOLCANISM; EXPLOSIVITY; HOLOCENES; ICELANDICS; ICELANDS; INTRUSIVE ROCKS; MELT INCLUSIONS; METEORIC WATERS; MGO CONTENT; OXYGEN FUGACITY; PHASE RELATIONSHIPS; QUENCHED MELTS; SILICIC MAGMAS; TECTONIC SETTINGS; VOLATILES;

DEGASSING; SUBMARINE GEOPHYSICS; VOLCANIC ROCKS; VOLCANOES;

OLIVINE;

EXPLOSIVE VOLCANISM; FRACTIONAL CRYSTALLIZATION; MAGMA; MELT INCLUSION; OLIVINE; VOLATILE ELEMENT; VOLCANIC ERUPTION;

HEKLA; ICELAND;

EID: 84867804087     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2012.09.047     Document Type: Article

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