The origin of hydrous, high-δ18O voluminous volcanism: Diverse oxygen isotope values and high magmatic water contents within the volcanic record of Klyuchevskoy volcano, Kamchatka, Russia

Contributions to Mineralogy and Petrology

Volumn 157, Issue 2, 2009, Pages 209-230

  Auer, Sara ^a   Bindeman, Ilya ^a   Wallace, Paul ^a   Ponomareva, Vera ^b   Portnyagin, Maxim ^c  

^a UNIVERSITY OF OREGON   (United States)

^b INSTITUTE OF VOLCANOLOGY AND SEISMOLOGY   (Russian Federation)

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

Author keywords

Hydrous melting; Ion microprobe; Melt inclusions; Olivine; Oxygen isotopes

Indexed keywords

BASALT; CHEMICAL COMPOSITION; CONCENTRATION (COMPOSITION); DEGASSING; IGNEOUS GEOCHEMISTRY; MELT INCLUSION; OLIVINE; OXYGEN ISOTOPE; PHENOCRYST; SUBDUCTION ZONE; TEPHRA; TEPHROCHRONOLOGY; TRACE ELEMENT; VOLCANIC ERUPTION; VOLCANISM; WATER CONTENT;

EURASIA; KAMCHATKA; KLYUCHEVSKOI VOLCANO; RUSSIAN FEDERATION;

EID: 57849161401     PISSN: 00107999     EISSN: None     Source Type: Journal    
DOI: 10.1007/s00410-008-0330-0     Document Type: Article

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