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...
المؤلفون الرئيسيون: | Prytulak, J, Elliott, T |
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التنسيق: | Journal article |
اللغة: | English |
منشور في: |
2007
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مواد مشابهة
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Doubly-distilling eclogite in ocean island basalt sources
حسب: Prytulak, J, وآخرون
منشور في: (2008) -
TiO2 in OIB and the preservation of extreme isotopic signatures
حسب: Prytulak, J, وآخرون
منشور في: (2007) -
Global isotopic signatures of oceanic island basalts / by
حسب: Oschmann, Lynn A
منشور في: (2010) -
Lithium isotope evidence for subduction-enriched mantle in the source of mid-ocean-ridge basalts.
حسب: Elliott, T, وآخرون
منشور في: (2006) -
Origin of 182W Anomalies in Ocean Island Basalts
حسب: Gregory J. Archer, وآخرون
منشور في: (2023-02-01)