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Therefore, various melts from basaltic to granitic compositions could be produced by partial melting of the metasomes in the mantle wedge and its underlying slab-mantle interface (Figure 8b).
Even andesitic melts could be produced by partial melting of a given mafic metasome that is generated by reaction of abundant felsic melts with the SSC peridotite (Chen et al. 2014).
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The concretes with silica fume were produced by partial substitution of cement with silica fume at varying amounts of 5 20%.
The RCC mixes were produced by partial substitution of cement with RHA at varying amounts of 3% and 5%.
The mixtures were produced by partial replacement of cement with the supplementary cementitious materials at different incorporation levels of 5, 10 and 20%.
Moreover, the SCCs with fly ash were produced by partial substitution of cement with fly ash at varying amounts of 20% to 60%.
A thermally stable and non-porous carbon material (SBET = 10 m2 g−1 and no micropores), with low ash content and basic character, was produced by partial carbonization of glycerol with sulphuric acid followed by calcination under inert atmosphere.
Thiol conjugates are produced by partial reduction of the interchain disulfides, followed by conjugation with a drug-linker, resulting in a heterogeneous mix of molecules that differ with respect to the site of conjugation and the number of drugs per antibody.
The in-situ Hf isotopic data indicate that most of the felsic magma was produced by partial melting of the lower crust, and that the intermediate magma witnessed intrusion of mafic magma derived from mantle with magma mixing in different proportion.
Event-related potential (ERP) signals measured at the scalp are produced by partial synchronization of neuronal field potentials across the cortex [1].
It was possible to estimate the H2O content in magmas by mixing the basalt magma, assumed to contain 0.5 wt% H2O (Tatsumi and Suzuki, 2009), with a rhyolitic magma that was produced by partial melting of the hydrous basalt.
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