Chemical complexity of hotspots caused by cycling oceanic crust through mantle reservoirs
نویسندگان
چکیده
Where ρ0, α0, ∆T , η, κ are dimensional reference values of density of the background mantle, thermal expansivity, temperature difference between core-mantle boundary and surface, reference viscosity at temperature T = 0.5 (non-dimensional), and thermal diffusivity, respectively. g and h are dimensional gravitational acceleration and thickness of mantle, respectively. 1 Chemical complexity of hotspots caused by cycling oceanic crust through mantle reservoirs SUPPLEMENTARY INFORMATION DOI: 10.1038/NGEO2120
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