²³⁸U-²³⁰Th-²²⁶Ra disequilibria constraints on the magmatic evolution of the cumbre vieja volcanics on la palma, Canary Islands

Keyphrases

• 226Ra 100%
• 230Th 100%
• 238U 100%
• Amphibole 40%
• Apatite 20%
• Basanite 20%
• Canary Islands 100%
• Clinopyroxene 20%
• Cumbre Vieja 100%
• Disequilibrium 100%
• Dynamic Melting 20%
• Element Pattern 20%
• Eruption Age 20%
• Fayalite 20%
• Fractional Crystallization 20%
• Garnet Lherzolite 20%
• H2O Content 20%
• Incompatible Trace Elements 20%
• Iron Oxide 20%
• La Palma 100%
• Lava 60%
• Liquid Line of Descent 20%
• Mafic 20%
• Mafic Lavas 20%
• Magma 20%
• Magma Batches 40%
• Magma Mixing 20%
• Magmatic Evolution 100%
• Melt-derived 20%
• MELTS Algorithm 20%
• Numerical Simulation 20%
• Oceanic Islands 20%
• Oxygen Fugacity 20%
• Parental Magma 20%
• Partial Melt 20%
• Partition Coefficient 20%
• Pb Isotopes 20%
• Phlogopite 20%
• Phonolite 20%
• Phonotephrite 20%
• Plagioclase 20%
• Plutonic Rocks 20%
• Pressure-temperature 20%
• Rapid Transport 20%
• Rift 20%
• Rift System 20%
• Silica 60%
• Sr-Nd Isotope Composition 20%
• Sr-Pb Isotopes 20%
• Syenite 20%
• Temperature Interval 20%
• Titanite 40%
• Trace Elements 20%
• Volcanic 100%

Earth and Planetary Sciences

• Amphibole 40%
• Basanite 20%
• Calcium Phosphate 20%
• Canary Island 100%
• Clinopyroxene 20%
• Fayalite 20%
• Fractional Crystallization 20%
• Fugacity 20%
• Garnet 20%
• Lherzolite 20%
• Magma 100%
• Partition Coefficient 20%
• Phlogopite 20%
• Phonolite 20%
• Plutonic Rock 20%
• Prehistoric 20%
• Syenite 20%
• Titanite 40%
• Trace Element 40%