Time constraints on the origin of large volume basalts derived from O-isotope and trace element mineral zoning and U-series disequilibria in the Laki and Grímsvötn volcanic system

Earth and Planetary Science Letters

Volumn 245, Issue 1-2, 2006, Pages 245-259

  Bindeman, Ilya N ^a   Sigmarsson, Olgeir ^b,c   Eiler, John ^d  

^a UNIVERSITY OF OREGON   (United States)

^b UNIVERSITÉ BLAISE PASCAL   (France)

^c UNIVERSITY OF ICELAND   (Iceland)

^d CALIFORNIA INSTITUTE OF TECHNOLOGY   (United States)

Author keywords

diffusion; Laki; oxygen isotopes; segregation; U series disequilibria

Indexed keywords

BASALTIC TEPHRA; DISEQUILIBRIUM PHENOCRYSTS; HOMOGENEOUS BASALTIC LAVAS; ICELANDIC MANTLE PLUME; OXYGEN ISOTOPE HETEROGENEITY; OXYGEN ISOTOPES; VOLCANIC SYSTEM;

DIFFUSION; HYDRATION; ISOTOPES; OLIVINE; OXYGEN; QUARTZ; TRACE ELEMENTS; VOLCANOES;

BASALT;

BASALT; FISSURE; OXYGEN ISOTOPE; TRACE ELEMENT; URANIUM SERIES DATING; VOLCANO; ZONING;

ARCTIC; ICELAND;

EID: 33646034303     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2006.02.029     Document Type: Article

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