Metasomatism of the crust-mantle boundary by melts derived from subducted sedimentary carbonates and silicates
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DOI: 10.1016/j.gca.2019.06.033
Abstract: Abstract Substantial quantities of sediments are known to enter the deep lithosphere at subduction zones, but the extent to which sediments melt and the process involved in sediment contribution to the deep lithosphere are inadequately… read more here.
Keywords: metasomatism crust; sedimentary carbonates; deep lithosphere; crust mantle ... See more keywords