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The NiO/SiO2 ratio of the silicate portion was 0.004.
The FeO/SiO2 mass ratio of the silicate portion was 0.67.
The composition of the silicate portion was determined by 10 randomly selected EPMA spots (10 μm spot diameter, Table 4).
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According to this model, the silicate portion of the Earth is composed of five dominant reservoirs: the depleted mantle (DM), the enriched mantle (EM), the lithospheric mantle (LM), the continental crust (CC), and the oceanic crust (OC).
Additional complexity may exist because in melts with mixed M m+ cations and H+, the H+, because of its size for steric reasons, exhibits preference for forming OH groups in the silicate portion of the network by reacting with the nonbridging oxygen in Q n species with the largest number of nonbridging oxygens (Cody et al. 2005).
Accessible Silicate Earth (part of the silicate Earth from which we can obtain materials for analysis).
Amphibole asbestos, a variety of the silicate mineral actinolite.
His work was one of the earliest contributions to the systematic study of the silicate minerals.
White mica, fine-grained variety of any of the silicate minerals muscovite, paragonite, or talc.
Amosite, a variety of the silicate mineral cummingtonite, which is a source of asbestos (see cummingtonite).
Summary of the silicate scale formation.
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