Evolution of Plate Tectonics on Earth since the Mid-Mesoarchean was Controlled by Sedimentary Fluxes from Continents to Oceans and Mantle Temperature

Stephan V Sobolev, GFZ Helmholtz Centre for Geosciences, Geodynamic Modelling Section, Potsdam, Germany and Michael Brown, University of Maryland, College Park, Laboratory for Crustal Petrology, Department of Geology, College Park, United States
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