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These rocks were formed by partial melting of lower continental crust.
This results because these rocks are differentiated by partial melting of the upper-mantle and oceanic-crust rock.
An origin by partial melting of high-pressure crustal sources seems unlikely from isotopic and trace element considerations.
They were possibly generated by partial melting of the thickened mafic lower continental crust.
These tonalities which occupied a mid-crustal position were generated by partial melting of lower crust.
Most magma formed by partial melting of the mantle is basaltic in composition, but, as it ascends, it assimilates silica, sodium, and potassium from the surrounding host rocks.
Similar(31)
This chemical separation by partial melting and outgassing of volatiles is termed differentiation.
This generation of ssRNA from dsRNA can be accomplished by the partial melting of the double-stranded helix, followed by the hybridization of RNA oligonucleotides to the resulting partially separated strand (Fig. 4).
The rising subduction-zone magma is probably basaltic in composition and is formed by the partial melting of mantle rocks.
Such a rhyolitic magma can be produced by ~10%% partial melting of the basaltic crust (Tatsumi and Suzuki, 2009).
The silicate melts generated by the partial melting of MORBs might thus undergo a structural transformation involving possible densification changes related to Si-O coordination states at depths of around ~2690 km, which is clearly shallower than the CMB.
More suggestions(15)
by partial inhibition of
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