Origins and Scales of Compositional Variations in Crustally Derived Granitic Rocks: The Example of the Dartmoor Pluton in the Cornubian Batholith of Southwest Britain

Keyphrases

• Pluton 100%
• Compositional Variation 100%
• Cornubian Batholith 100%
• Dartmoor 100%
• Granitic Rocks 100%
• Magma 66%
• Isotopic Heterogeneity 66%
• Source Terrane 66%
• Light Elements 66%
• Downscaling 33%
• Crystal Fractionation 33%
• Patchy 33%
• Sampling numbers 33%
• Partial Melting 33%
• Granitic Magma 33%
• Protolith 33%
• Silicic 33%
• S-type 33%
• Plutonic Rocks 33%
• Silica 33%
• Magma Source 33%
• Plagioclase 33%
• Granitic Pluton 33%
• Aplite 33%
• Magma Genesis 33%
• Syn-collisional 33%
• O Isotopes 33%
• Peritectic 33%
• Granitic Intrusions 33%
• Lithological Variations 33%
• Aqueous Fluid 33%
• Orthopyroxene 33%
• Low Density 33%
• Ilmenite 33%
• Major Minerals 33%
• Metapelite 33%
• Magmatic Melt 33%
• Mechanical Mixing 33%
• Chemical Variation 33%
• Variable Proportion 33%
• Entrainment 33%
• Post-orogenic 33%
• Rock Forms 33%
• Flow-based 33%
• Small-scale Heterogeneity 33%
• Mica 33%
• Middle Crust 33%
• Whole Rock 33%
• Sampling Scale 33%
• Shallow Crust 33%
• H2O Content 33%
• Metavolcanic Rocks 33%
• Microgranite 33%

Earth and Planetary Sciences

• Magma 100%
• United Kingdom 100%
• Batholith 100%
• Fractionation 75%
• Terrane 50%
• Light Element 50%
• Partial Melting 25%
• Protolith 25%
• Plutonic Rock 25%
• Aplite 25%
• Metavolcanic Rock 25%
• Orthopyroxene 25%
• Metapelite 25%
• Ilmenite 25%