Keyphrases
Silicate Earth
100%
Stable Isotope Ratios
100%
Melt Depletion
100%
Zirconia
100%
Isotope Fractionation
100%
Zircon
75%
Mantle Source
50%
Silica
50%
Limited Range
50%
Iceland
50%
Ocean Island Basalt
50%
Mantle Melting
50%
Melt Extraction
50%
Hekla Volcano
50%
Mass-dependent
50%
Chondrites
25%
Residual Melt
25%
Fractionation Effect
25%
Isotopic Variation
25%
Low Coordination
25%
Isotope Composition
25%
Felsic Crust
25%
Whole Rock
25%
Depleted Mantle
25%
Lava
25%
Stable Isotopes
25%
Primitive Mantle
25%
Double Spike
25%
Partial Melt
25%
Coordination Chemistry
25%
Isotope Measurements
25%
Orthopyroxene
25%
Depletion Event
25%
Light Isotopes
25%
Zircon Saturation Temperature
25%
Igneous Rocks
25%
Mass-dependent Fractionation
25%
Crust Formation
25%
Earth and Planetary Sciences
Fractionation
100%
Magmatic Differentiation
100%
Stable Isotope
100%
Isotopic Fractionation
100%
Zircon
80%
Mid-Ocean Ridge Basalt
80%
Ocean Island Basalt
40%
Mantle Source
40%
Iceland
40%
Orthopyroxene
20%
Chondrite
20%
Igneous Rock
20%