Plate tectonics in action in the Mesoarchean: Implication from the Olondo greenstone belt on the Aldan Shield of Siberian Craton

Keyphrases

• Aging Model 10%
• Aldan Shield 100%
• Archean 20%
• Boninite 10%
• Cratons 10%
• Cumulate 10%
• Deep Mantle 10%
• Dunite 50%
• Formation Age 10%
• Formation Settings 10%
• Garnet Stability 10%
• Geochemical Characteristics 10%
• Geochemical Data 10%
• Greenstone Belt 100%
• Initiation Mechanism 10%
• Isotopic Composition 10%
• Isotopic Data 10%
• Komatiitic Basalt 20%
• Light Rare Earth 10%
• Mafic Rocks 30%
• Mantle Plume 20%
• Mantle Source 30%
• Mesoarchean 100%
• Metasomatism 10%
• Mid-ocean Ridge 10%
• N-MORB 10%
• Nb-Ta 20%
• Partial Melting 10%
• Pattern with Variables 10%
• Plate Tectonics 100%
• Platinum Group Elements 10%
• Plume 10%
• Plume-induced Subduction Initiation 10%
• Rare Earth Element Pattern 30%
• Rhenium-osmium 10%
• Seafloor Spreading 10%
• Siberia 10%
• Siberian Craton 100%
• Siderophile Elements 10%
• Stability Field 10%
• Subduction 10%
• Subduction-related 20%
• Supra-subduction Zone Ophiolite 10%
• Tectonic Processes 10%
• Tholeiitic Basalt 20%
• Ultramafic 10%
• Ultramafic Rocks 50%

Earth and Planetary Sciences

• Basalt 10%
• Boninite 10%
• Craton 100%
• Dunite 50%
• Garnet 10%
• Greenstone Belt 100%
• Isotopic Composition 10%
• Mafic Rock 50%
• Mantle Plume 20%
• Mantle Source 30%
• Metasomatism 10%
• Mid-Ocean Ridge 10%
• Mid-Ocean Ridge Basalt 10%
• Ophiolite 10%
• Partial Melting 10%
• Plate (Tectonics) 100%
• Platinum Group Element 20%
• Rare Earth Element 30%
• Rhenium 10%
• Sea Floor Spreading 10%
• Siberia 10%
• Siderophile Element 10%
• Subduction Zone 10%
• Tholeiitic Basalt 20%
• Ultramafic Rock 30%