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A felsic end to Bushveld differentiation
Jill A. Vantongeren
, Edmonda A. Mathez
, Peter B. Kelemen
Research output
:
Contribution to journal
›
Article
›
peer-review
96
Scopus citations
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Keyphrases
Bushveld
100%
Upper Zone
100%
Main Zone
100%
Magma
75%
Cumulate
75%
Trace Elements
50%
Orthopyroxene
50%
Parent Magma
50%
Rooiberg Group
50%
Felsic Volcanic Rocks
50%
Lava
25%
Isotopic Composition
25%
Magma Chamber
25%
Bulk Composition
25%
Magma Composition
25%
Thermodynamic Modeling
25%
Rooiberg
25%
Granophyre
25%
Trace Element Composition
25%
Major Element Composition
25%
Genetic Link
25%
Bushveld Igneous Complex
25%
Magma Volume
25%
Earth and Planetary Sciences
Magma
100%
Trace Element
50%
Volcanic Rock
33%
Orthopyroxene
33%
Isotopic Composition
16%
Magma Chamber
16%
Granophyre
16%