Origin of HIMU and EM-1 domain sampled by ocean island basalts, kimberlites and carbonatites: The role of CO2- fluxed lower mantle melting in thermochemical upwellings
| Data(s) |
2010
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|---|---|
| Identificador | |
| Publicador |
Elsevier BV |
| Relação |
DOI:10.1016/j.pepi.2010.05.008 Collerson, Kenneth, Williams, Quentin, Ewart, A, & Murphy, David (2010) Origin of HIMU and EM-1 domain 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, 181(3-4), pp. 112-131. |
| Fonte |
Biogeoscience; Faculty of Science and Technology |
| Palavras-Chave | #040200 GEOCHEMISTRY #040300 GEOLOGY #Mantle Heterogeneity, Em, HIMU, kimberlite, Carbonatite, Ocean island basalt, modelling lower mantle melting, buoyant melts and residues, Carbon dioxide |
| Tipo |
Journal Article |
