TiO2 enrichment in ocean island basalts
An extensive dataset of ocean island basalt (OIB) compositions highlight that their titanium (Ti) contents are generally too high to be derived from melting of a peridotitic mantle. Even vanishingly small degree melts of a primitive mantle source have insufficient Ti to reproduce the compositions of...
Κύριοι συγγραφείς: | Prytulak, J, Elliott, T |
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Μορφή: | Journal article |
Γλώσσα: | English |
Έκδοση: |
2007
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Παρόμοια τεκμήρια
Παρόμοια τεκμήρια
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Doubly-distilling eclogite in ocean island basalt sources
ανά: Prytulak, J, κ.ά.
Έκδοση: (2008) -
TiO2 in OIB and the preservation of extreme isotopic signatures
ανά: Prytulak, J, κ.ά.
Έκδοση: (2007) -
Global isotopic signatures of oceanic island basalts / by
ανά: Oschmann, Lynn A
Έκδοση: (2010) -
Lithium isotope evidence for subduction-enriched mantle in the source of mid-ocean-ridge basalts.
ανά: Elliott, T, κ.ά.
Έκδοση: (2006) -
Origin of 182W Anomalies in Ocean Island Basalts
ανά: Gregory J. Archer, κ.ά.
Έκδοση: (2023-02-01)