Submarine and subaerial lavas in the West Antarctic Rift System: Temporal record of shifting magma source components from the lithosphere and asthenosphere

Keyphrases

• Subduction 100%
• Lava 100%
• Asthenosphere 100%
• Temporal Records 100%
• Submarine 100%
• Magma Source 100%
• West Antarctic Rift System 100%
• Lithology 66%
• Decompression Melting 66%
• Ross Sea 66%
• Rift 33%
• Tectonics 33%
• Rifting 33%
• Pyroxenite 33%
• West Antarctica 33%
• Terror 33%
• Plume 33%
• Southern Ocean 33%
• Competing Models 33%
• Upwelling 33%
• Ocean Island Basalt 33%
• Source Area 33%
• Endmember 33%
• Lithospheric Mantle 33%
• Gondwana 33%
• U-Pb 33%
• Oxide Composition 33%
• Compositional Structure 33%
• Ingrowth 33%
• Amphibole 33%
• Mantle Source 33%
• Petrogenesis 33%
• Cenozoic 33%
• Seamount 33%
• Embayment 33%
• Major Oxides 33%
• Beaufort 33%
• Melting Model 33%
• Generation Model 33%
• Flux Melting 33%
• Active Margin 33%
• Geochemical Information 33%
• Low-velocity Anomaly 33%
• Northern Victoria Land 33%
• Trace Element Signature 33%
• Alkaline Magmas 33%
• Magma Generation 33%
• Metasomatized Peridotite 33%
• Mt. Melbourne 33%
• Cenozoic Extension 33%
• Paleo-Pacific 33%
• Tectonomagmatic 33%

Earth and Planetary Sciences

• Lithosphere 100%
• Asthenosphere 100%
• Magma 100%
• Temporal Record 100%
• Pressure Reduction 100%
• Tectonics 50%
• Antarctic Region 50%
• Southern Ocean 50%
• Peridotite 50%
• Trace Element 50%
• Pyroxenite 50%
• Ocean Island Basalt 50%
• Rifting 50%
• Petrogenesis 50%
• Gondwana 50%
• Amphibole 50%
• Mantle Source 50%
• Seamount 50%
• Active Margin 50%
• Magma Generation 50%