Zircon rare earth element (REE) oxy-barometers have been widely used to calculate magma
oxygen fugacity. However, sometimes confusing results are obtained, such as extremely …

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 …

Abstract The Cuonadong Sn-W-Be polymetallic deposit is the first Cenozoic leucogranite-
related rare-metal deposit with giant metallogenic potential in the Himalayan orogen …

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 …

Subduction initiation is a key process in the operation of plate tectonics. Our understanding
of melting processes and magmatic evolution during subduction initiation has largely been …

The lithosphere provides a reservoir for ore-forming elements introduced by repeated
fertilisation during asthenosphere-lithosphere interaction by the slab subduction. Here we …

Magmatic arcs are natural laboratories for studying the growth of continental crusts. The
Gangdese arc, southern Tibet, is an archetypal continental magmatic arc that formed due to …

位于青藏高原南部的冈底斯岩浆弧是新特提斯大洋岩石圈长期俯冲导致的中生代岩浆作用的
产物, 而且在印度与亚洲大陆碰撞过程中叠加了**烈的新生代岩浆作用, 是世界上典型的复合型 …

Abstract The Demingding Cu–Mo deposit, found in the eastern Gangdese metallogenic belt
in China, has a significant exploration potential. Detailed field studies coupled with short …

The genetic mechanism and exploration model for porphyry deposits in subduction zones
has been comprehensively and systematically investigated; in contrast, our understanding …