The somuncura large igneous province in Patagonia: Interaction of a transient mantle thermal anomaly with a subducting slab

Keyphrases

• Patagonia 100%
• Isotopic Signature 100%
• Large Igneous Provinces 100%
• Thermal Anomaly 100%
• Subducting Slab 100%
• Mantle Upwelling 66%
• Sr-Nd 66%
• Mafic 66%
• Rare Earth Element Pattern 66%
• Intraplate 66%
• South America 33%
• Crustal Contamination 33%
• Heavy Rare Earth Elements 33%
• Back-arc 33%
• Depleted Mantle 33%
• Plume 33%
• Tholeiitic 33%
• Isotopic Data 33%
• Magmatism 33%
• Trace Elements 33%
• Arc-like 33%
• Hydrous 33%
• Sr-Nd-Pb 33%
• Low Volume 33%
• High Field Strength Elements 33%
• Magma Source 33%
• Volcanic Field 33%
• Oligo-Miocene 33%
• Tristan Da Cunha 33%
• Subducting Plate 33%
• Mantle-derived Magma 33%
• Plate Reorganization 33%
• Mantle Components 33%
• Subduction-related 33%
• Mafic Volcanics 33%
• Pb Isotopes 33%
• Related Components 33%
• Incompatible Elements 33%
• Elemental Abundances 33%
• Subduction 33%

Earth and Planetary Sciences

• Mantle Upwelling 100%
• Large Igneous Province 100%
• Temperature Anomaly 100%
• Rare Earth Element 100%
• Miocene 50%
• Crustal Contamination 50%
• Magma 50%
• Trace Element 50%
• Magmatism 50%
• Paleogene 50%
• Field Strength 50%
• South America 50%