The effects of heterogeneity in magma water concentration on the development of flow banding and spherulites in rhyolitic lava

Journal of Volcanology and Geothermal Research

Volumn 183, Issue 3-4, 2009, Pages 157-169

  Seaman, Sheila J ^a   Dyar, M Darby ^b   Marinkovic, Nebojsa ^c  

^a UNIVERSITY OF MASSACHUSETTS   (United States)

^b MOUNT HOLYOKE COLLEGE   (United States)

^c BROOKHAVEN NATIONAL LABORATORY   (United States)

Author keywords

flow banding; FTIR spectroscopy; rhyolite; spherulite; water

Indexed keywords

23 MILLION; ALTERNATING LAYERS; ARIZONA; FLOW BANDING; FOURIER TRANSFORM INFRARED; FTIR SPECTROSCOPY; INTERGROWTH; LAVA FLOWS; RHYOLITE; RHYOLITIC LAVAS; SANIDINE; SPHERULITE; WATER AVAILABILITY; WATER CONCENTRATIONS;

CRYSTALS; FOURIER TRANSFORM INFRARED SPECTROSCOPY; GLASS; GRAIN BOUNDARIES; GRANITE; INFRARED RADIATION; OXIDE MINERALS; QUARTZ; QUENCHING; TEXTURES;

CONCENTRATION (PROCESS);

FTIR SPECTROSCOPY; LAVA FLOW; MAGMA; RHYOLITE; SPHERULITE; WATER;

ARIZONA; NORTH AMERICA; SYCAMORE CANYON; UNITED STATES;

EID: 67349265922     PISSN: 03770273     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jvolgeores.2009.03.001     Document Type: Article

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