Transition from Vertical to Horizontal Tectonic Regime During the Paleoarchean-Mesoarchean: Evidence from Mafic-Ultramafic Rocks of the Holenarsipur Greenstone Belt, Western Dharwar Craton, Southern India
PRECAMBRIAN RESEARCH(2024)
Key words
Archean mantle,Dharwar Craton,Greenstone belts,Plate tectonics,Serpentinization,Ultramafics
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