Northeast (NE) China lies in the eastern sector of the Central Asian Orogenic Belt (CAOB)
that connects with the Circum-Pacific Orogenic Belt in the east, and accommodates …

Abstract The Dabie Shan in central East China is a collisional orogenic belt suturing the
North China and Yangtze blocks. It was formed by Jurassic-Early Cretaceous continental …

In this contribution we discuss a series of porphyry and porphyry-skarn mineral systems,
which constitute important metallogenic belts along major lithospheric breaks and/or …

Abstract The Qinling Orogen in central China is a complex collage built through the closure
of the northernmost Paleo-Tethys and the suturing of the Yangtze and the North China …

Sulfur and chlorine are the two most important ligands accounting for metal transport in the
upper crust. In this study, four metal-and sulfur-saturated model fluids with varying salinities …

As one of the most important Mo provinces in the world, the Qinling Orogen is host to mainly
Late Mesozoic (Late Jurassic–Early Cretaceous) porphyry Mo systems. Recently, additional …

Abstract The Sha**gou porphyry Mo deposit, one of the largest Mo deposits in Asia, is
located in the Dabie Orogen, Central China. Hydrothermal alteration and mineralization at …

Abstract The Luoboling Cu–Mo deposit in the Zi**shan Orefield, Fujian province,
southeastern China, is a large porphyry deposit hosted by the Sifang granodiorite and the …

Abstract The Yuchiling Mo deposit is a recently discovered giant porphyry system in the East
Qinling Mo belt, China. Its apparent causative intrusion, ie, the Yuchiling granite porphyry, is …

Abstract The giant Donggebi porphyry Mo deposit is located in the Jueluotage metallogenic
belt of Eastern Tianshan, **njiang, Northwest China. Mo mineralization mainly occurs as …