Granite petrogenesis is associated with the formation and evolution of continental crust
along convergent plate boundaries. While magmatic processes such as partial melting and …

Tungsten and Sn display similar behavior during magmatic processes and are commonly
associated spatially and genetically with highly evolved granites. Nonetheless, they typically …

Understanding the processes of subducted sediment recycling in subduction zones is vital to
decipher Earth's crust-mantle interactions. This study uses along-arc geochemical variations …

The property of regional metamorphism at convergent plate margins is substantially related
to the change of geothermal gradients, resulting in different types of crustal reworking …

Zirconium is one of high field strength elements but its isotope behavior during geochemical
processes is still uncertain because of the limited database. While Zr isotopes in magmatic …

The production of granitic melts by decompressional melting of deeply subducted crustal
rocks under high-pressure (HP) to ultrahigh-pressure (UHP) conditions is important for the …

It remains unresolved whether extensive granitoids can originate from ultrahigh‐temperature
crustal anatexis beyond the stability of fusible hydrous minerals and, if any, how they are …

Two generations of garnet are recognized in a granite and a pegmatite from the Gangdese
orogen in southeastern Tibet on the basis of a combined study of petrography, major and …

Abstract Exhumed (ultra) high-pressure ([U] HP) metamorphic rocks are markers of paleo-
subduction zones and can provide crucial implications for the geodynamic evolution of …

Abstract Sitting between the Greater Himalayan sequence (GHS) and Lesser Himalayan
sequence (LHS), the Main Central Thrust zone (MCTZ) has experienced multiple episodes …