Water-fluxed melting, also known as fluid-or water-present melting, is a fundamental process
in the differentiation of continents but its importance has been underestimated in the past 20 …

Many granites result from anatexis of common crustal rock types and the segregation,
aggregation, ascent and emplacement of the resultant magma. What then is the connection …

Ultrahigh temperature (UHT) metamorphism is the most thermally extreme form of regional
crustal metamorphism, with temperatures exceeding 900° C. UHT crustal metamorphism is …

At low temperatures (< 750 C at moderate to high crustal pressures), the production of
sufficient melt to reach the melt connectivity transition (∼ 7 vol%), enabling melt drainage …

The origin of different kinds of granitic rocks is examined within the framework of
experimental studies of melting of metamorphic rocks, and of reaction between basaltic …

Zircon saturation temperatures (T Zr) calculated from bulk-rock compositions provide
minimum estimates of temperature if the magma was undersaturated, but maxima if it was …

The melting relations of five metamorphosed basalts and andesites (greenstones and
amphibolites), collected from the late Jurassic Smartville arc complex of California, were …

Page 1 Minerals and Rocks Wilhelm Johannes François Holtz Petrogenesis and Experimental
Petrology of Granitic Rocks $ Springer-Verlag Page 2 Minerals and Rocks 22 Editor in Chief PJ …

We have melted metapelitic rocks from the High Himalayan Crystalline Sequence that are
likely sources of leucogranite magmas. Starting materials were a muscovite schist and a …

Peraluminous granitoid magmas are a characteristic product of ultrametamorphism leading
to anatexis of aluminous metasedimentary rocks in the continental crust. The mechanisms …