In-situ analysis of minerals, such as zircon hafnium (Hf) and oxygen (O) isotopes, has been
pivotal in investigating magmatic evolution and related ore systems. In order to better …

Igneous complexes with a wide variety of lithologies in continental magmatic arcs provide a
critical insight into the composition and formation mechanism of continental crust. We report …

Jurassic arc magmatic rocks are widely distributed along the Gangdese belt, southern Tibet,
however, only one Jurassic arc-related porphyry Cu deposit (the Xietongmen deposit) has …

The Jurassic magmatism distributed in the southern Lhasa subterrane (SLT) has been
recognized as a record of the early-stage evolution of the Neo-Tethys ocean; however, the …

Mafic microgranular enclaves (MMEs), widespread in intermediate to felsic arc plutons, carry
significant information on the genesis and evolution of arc magmas, yet their origin remains …

Jurassic adakitic rocks in the southern Lhasa subterrane are relatively rare, poorly
documented, and their petrogenesis and geodynamic setting are unclear. To explore these …

Abstract The Tibetan Plateau is one of the most significant Cu poly-metallic mineralization
regions in the world and preserves important information related to subductional and …

The co-existence of Cretaceous adakitic and A-type granitoids in southern Tibet can offer
fundamental constraints on subduction of the Neo-Tethyan oceanic plate and associated …

Abstract The Lakang'e porphyry Mo (Cu) deposit, intermediate to large in size, is located in
the eastern part of the southern Gangdese metallogenic belt. It is associated with a Miocene …

The Gangdese belt is among the most significant magmatic and metallogenic belts in the
world. The multistage magmatism that generated the deposits in the Gangdese is a major …