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- W2006185623 abstract "Two processes may transport material across the boundary between lower continental crust and upper mantle: (a)Relatively dense picritic magmas may be trapped at or near the base of the crust where they become contaminated with lower crustal wall rocks and differentiate to form layered sills with gabbroic upper parts and olivine + pyroxene cumulate lower parts. The siliceous, aluminous, incompatible-element enriched gabbroic rocks have relatively low densities and are incorporated in the continental crust; the ultramafic cumulates have higher densities than lower crustal and upper mantle rocks and sink into the mantle carrying with them lower crustal contaminant. (b) Granitoid magmas formed during intracrustal melting leave dense restite minerals which also return to the mantle. These crustal foundering processes result in (a) the building of continental crust; (b) enrichment of continental lithospheric mantle with material from the lower continental crust; (c) formation of sources for certain oceanic island basalts." @default.
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- W2006185623 date "1989-04-01" @default.
- W2006185623 modified "2023-10-18" @default.
- W2006185623 title "An open boundary between lower continental crust and mantle: its role in crust formation and crustal recycling" @default.
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- W2006185623 doi "https://doi.org/10.1016/0040-1951(89)90154-6" @default.
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