Widespread anatexis was a regional response to the evolution of the Himalayan‐Tibetan
Orogen that occurred some 30 Ma after collision between Asia and India. This paper reviews …

With less than two decades of activity, research on melt inclusions (MI) in crystals from rocks
that have undergone crustal anatexis–migmatites and granulites–is a recent addition to …

Granitoids are a major component of the continental crust. They play a pivotal role in its
evolution, either by adding new material (continental growth), or by reworking older …

Partial melting of deep continental crust may occur during either prograde heating or
decompression. Although the effect of temperature on crustal melting has been widely …

Petrological evidence is provided for partial melting of ultrahigh-pressure (UHP)
metamorphic granitic gneiss in the Sulu orogen. Petrographic observations show the …

To better understand the formation of high-temperature metamorphic rocks, we present a
detailed petrological and geochronological study of recently discovered cordierite-bearing …

This review presents a compositional database of primary anatectic granitoid magmas,
entirely based on melt inclusions (MI) in high-grade metamorphic rocks. Although MI are …

Inclusions in minerals, whether fluids, melts or crystalline phases, are small pieces of the
large-scale puzzle of Nature, time-consuming to investigate and often of difficult …

Monazite is a key accessory mineral for metamorphic geochronology, but interpretation of its
complex chemical and age zoning acquired during high-temperature metamorphism and …

The timing of crustal melting and cooling has been investigated across the migmatites of the
Greater Himalayan Crystalline Complex (GHC) in the Nyalam region, central Himalaya …