Origin of HIMU and EM-1 domains sampled by ocean island basalts, kimberlites and carbonatites: The role of CO2-fluxed lower mantle melting in thermochemical upwellings

Physics of the Earth and Planetary Interiors

Volumn 181, Issue 3-4, 2010, Pages 112-131

  Collerson, Kenneth D ^a   Williams, Quentin ^b   Ewart, Anthony E ^a   Murphy, David T ^c  

^a UNIVERSITY OF QUEENSLAND   (Australia)

^b UNIVERSITY OF CALIFORNIA   (United States)

^c QUEENSLAND UNIVERSITY OF TECHNOLOGY   (Australia)

Author keywords

Buoyant melts and residues; Carbon dioxide; Carbonatite; EM; HIMU; Kimberlite; Mantle heterogeneity; Modelling lower mantle melting; Ocean island basalt

Indexed keywords

CARBONATITES; HIMU; LOWER MANTLE; MANTLE HETEROGENEITY; OCEAN ISLAND BASALTS;

BASALT; BUOYANCY; CARBON DIOXIDE; GEOCHRONOLOGY; INERT GASES; ISOTOPES; MINERALS; OCEANOGRAPHY; SEDIMENTS; TECTONICS;

MELTING;

CARBON DIOXIDE; CARBONATITE; COMPUTER SIMULATION; IGNEOUS GEOCHEMISTRY; ISOTOPIC COMPOSITION; ISOTOPIC RATIO; KIMBERLITE; LOWER MANTLE; MANTLE CHEMISTRY; MANTLE PLUME; NUMERICAL MODEL; OCEAN ISLAND BASALT; OCEANIC CRUST; OCEANIC LITHOSPHERE; PARENT BODY; PARTIAL MELTING; PARTITION COEFFICIENT; QUANTITATIVE ANALYSIS; THERMOCHEMISTRY;

EID: 77954817104     PISSN: 00319201     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.pepi.2010.05.008     Document Type: Article

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