Barometry of lavas from the 1951 eruption of Fogo, Cape Verde Islands: Implications for historic and prehistoric magma plumbing systems

Journal of Volcanology and Geothermal Research

Volumn 217-218, Issue , 2012, Pages 73-90

  Hildner, Elliot ^a   Klügel, Andreas ^a   Hansteen, Thor H ^b  

^a UNIVERSITY OF BREMEN   (Germany)

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

Author keywords

Cape Verde; Flank collapse; Fluid inclusion microthermometry; Fogo; Geochemistry; Magma plumbing; Thermobarometry

Indexed keywords

CAPE VERDE; FLANK COLLAPSE; FLUID INCLUSION MICROTHERMOMETRY; FOGO; THERMOBAROMETRY;

BAROMETERS; CARBON DIOXIDE; GEOCHEMISTRY; IGNEOUS ROCKS; MINERALOGY; OLIVINE; SOLID SOLUTIONS; VOLCANOES; WATER PIPING SYSTEMS;

PLUMBING;

BAROMETRY; CLINOPYROXENE; CRYSTALLIZATION; FLUID INCLUSION; GEOCHEMISTRY; LAVA; MAGMA; MAGMA CHAMBER; PHENOCRYST; VOLCANIC ERUPTION; VOLCANISM; XENOLITH;

CAPE VERDE; FOGO;

EID: 84856186969     PISSN: 03770273     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jvolgeores.2011.12.014     Document Type: Article

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