Subduction Zones Cocos Plate Seismic Monitoring Indian and Eurasian Plates Seismic Events Seismic Waves Seismic Zones Indian Plate San Andreas Fault Seismicity Eurasian Plate Pacific Plate Seismic Activity Earthquake Mechanics Pacific Ring of Fire Seismic Studies Nazca Plate Earthquakes Himalayas Nazca and South American Plates Caribbean and South American Plates Caribbean Plate Cinturón de Fuego Ring of Fire Cocos and Caribbean Plates Cocos Plate Interaction Seismic Research Eurasian and Indian Plates Mendocino Triple Junction Earthquake Zones Convergent Boundaries Fault Lines Pacific and North American Plates Cocos and North American Plates Gulf of California Caribbean Region Indo-Australian and Eurasian Plates Earthquake Swarms Earthquake Analysis Earthquake Preparedness Strike-Slip Faults North Anatolian Fault Strike-Slip Boundaries Philippine Sea Plate Indian Plate and Eurasian Plate Myanmar Hindu Kush Anatolian Plate Euroasiatic and African Plates African and Eurasian Plates Earthquake Risk Cinturón de Fuego del Pacífico Philippine Trench Seismic Risk Makran Subduction Zone Arabian Plate North Atlantic Plate Movements Hindu Kush Region Himalayan Region Earthquake Magnitude Kafue Rift Eurasian and African Plates African Plate Scotia and South American Plates Caribbean and South America Alboran Sea Faulting South American Plate Earthquake Occurrence Pacific Plate Interaction
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The findings provide the first geochemical proof of mantle-to-surface flow in the Kafue Rift.
