Abstract Most magmatic Ni–Cu–PGE sulphide deposits occur within long-lived magma
pathways fed by high degree partial melts of the mantle. Holistic mineral-system analysis for …

In this paper we present a review of mineral systems in northern Xinjiang, NW China,
focussing on the Tianshan, West and East Junggar and Altay orogenic belts, all of which are …

The importance of externally derived sulfur in the genesis of sulfide-rich, magmatic Ni-Cu-
(platinum group element [PGE]) deposits remains a key, yet unresolved, issue. Calculations …

This paper reports the first set of data for the newly-discovered Xiarihamu magmatic Ni–Cu
sulfide deposit in the Eastern Kunlun Paleozoic arc terrane which is located in the northern …

A large proportion of ores in magmatic sulfide deposits consist of mixtures of cumulus
silicate minerals, sulfide liquid, and silicate melt, with characteristic textural relationships that …

Large areas of central Asia and mainland China have been affected by intraplate
anorogenic magmatism, linked to mantle activity from the Palaeoproterozoic to present day …

This chapter focuses on S in porphyry-type ore deposits, layered-mafic-intrusion-hosted ore
bodies, and magmatic sulfide deposits. Porphyry-type ore deposits, eg, Bingham Canyon …

Addition of crustal sulfur to the Jinchuan magma or oxidation of the magma associated with
carbonate assimilation has been considered to be the main cause of sulfide saturation in the …

The Jinchuan deposit, NW China, is one of the world's most important Ni-Cu-(PGE) sulfide
deposits related to a magma conduit system and is hosted in an ultramafic intrusion. The …

Abstract The Jinchuan Ni-Cu-(PGE) deposit is the largest single magmatic Ni deposit in the
world. It is hosted by a small ultramafic intrusion in the Longshoushan terrane located in the …