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Magma evolution in a Proterozoic rifting environment.
D. Francis, J. Ludden, A. Hynes
Institute for GeoEnergy Engineering
School of Energy, Geoscience, Infrastructure and Society
Research output
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Contribution to journal
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Article
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peer-review
69
Citations (Scopus)
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Earth and Planetary Sciences
Rifting
100%
Magma
100%
Magma Evolution
100%
Basalt
88%
Olivine
55%
Pyroxene
33%
Fractionation
33%
Stratigraphy
11%
Oceanic Crust
11%
Clastic Sediment
11%
Andesite
11%
Continental Crust
11%
Volcanic Rock
11%
Mantle Source
11%
Clinopyroxene
11%
Quebec
11%
INIS
environment
100%
magma
100%
basalt
80%
olivine
50%
fractionation
30%
pyroxenes
30%
crystals
20%
pools
20%
plagioclase
20%
levels
10%
filters
10%
surfaces
10%
failures
10%
sediments
10%
margins
10%
geochemistry
10%
segregation
10%
assimilation
10%
stratigraphy
10%
feldspars
10%
oceanic crust
10%
quebec
10%
volcanic rocks
10%
continental crust
10%
andesites
10%