Petrogenesis of the Neoproterozoic West Highland Granitic Gneiss, Scottish Caledonides: cryptic mantle input to S-type granites?

Earth and Planetary Sciences

• Affinity 33%
• Alternative 33%
• Analogy 33%
• Attribution 33%
• Constraint 33%
• Crust 33%
• Dating 33%
• Entrainment 33%
• Geochemistry 33%
• Geological Fault 33%
• Gneiss 100%
• Granite 66%
• Host 33%
• Incorporation 33%
• Input 66%
• Institution 33%
• Isotope 33%
• Isotope Ratios 33%
• Magma 66%
• Mantle 66%
• Melt 33%
• Metabasite 33%
• Metasediment 66%
• Meteoric Water 33%
• Mid-Ocean Ridge Basalt 33%
• Model 33%
• Oxygen 33%
• Partial Melting 33%
• Petrogenesis 33%
• Protolith 33%
• Rare Earth Element 33%
• Restite 33%
• Scotland 33%
• Show 33%
• Support 33%
• Terrane 33%
• Trace Element 33%

INIS

• affinity 33%
• constraints 33%
• entrainment 33%
• geochemistry 33%
• gneisses 33%
• granites 66%
• hafnium isotopes 33%
• host 33%
• interactions 33%
• isotope ratio 33%
• juveniles 33%
• magma 66%
• melting 66%
• meteoric water 33%
• mixing 33%
• neodymium isotopes 33%
• origin 33%
• oxygen isotopes 33%
• petrogenesis 33%
• scotland 33%
• strontium isotopes 33%
• trace elements 33%