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Richard A. Meisch,Marilyn E. Carrollng rock. This means that metamorphic . will rarely exceed 850°–900°C during a first, major, thermal event. At this stage, crustal magma production will depend on the fertility of the source rock and the intensity of the thermal anomaly responsible for the metamorphism. With a fertile lower crust, su

abnegate

Peter Bult,Nicoline Hoogerbrugge0.16; while in Satnuru, they are comparable, i.e. 0.14–0.20 and 0.13–0.18 respectively. This suggests that .. in the Madras rocks were controlled internally and in Satnuru rocks externally. Algebraic analysis following Gibbs’ method shows that .. decreases with increasing X.(Bt) in charnockites of b

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Genesis of Continental Crust: Evidence from Island Arcs, Granulites, and Exospheric Processes the mantle. Thinner overriding lithosphere in Archean collision zones would have allowed dehydration melting of hydrated, subducted basic protoliths and direct production of Na-rich granitoids. Accumulation of sedimentary mass, cannibalistic recycling and intracrustal melting driven by under- and i

echnic

The Granulite — Granite Connexionnous granitoids. Non-restitic, mafic granulites represent basaltic magma that provided the heat source for metamorphism and melting of the overlying rocks. Restitic granulites are the refractory, residual complements of the granitoid magmas emplaced at higher levels. Silicic magmatism is most common

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