Planetary Mantle Composition is a geochemical construct that specifies the relative abundances of elements and minerals within the silicate-rich interior layer of a planetary body, distinguishing it from other planetary reservoirs by its physical state, differentiation history, and role in magmatic and tectonic processes.
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Water in Earth's Mantle: The Role of Nominally Anhydrous Minerals
David Bell, George R. Rossman · Science · 1992 · 954 citations
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Planetary Science Institute
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