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 …

High resolution X-ray computed tomography (CT) is the industrial equivalent of medical CAT
scanning and provides a mechanism for non-destructive studies of the three-dimensional …

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 …

A common feature of the mineralised chonolith intrusions of the Norilsk-Talnakh camp is the
presence of globular disseminated Ni–Cu–Fe sulphide ores, particularly well developed …

For decades, there has been debate surrounding the transport of dense metal-rich sulfide
liquid in mafic magmas. This topic is crucial to understanding the genesis of valuable …

High-resolution X-ray computed tomography (HRXCT) is a nondestructive technique that
allows exploration of the three-dimensional distribution of minerals and pore space in …

Ore forming processes involve the redistribution of heat, mass and momentum by a wide
range of processes operating at different time and length scales. The fastest process at any …

The physics and chemistry of ore formation in magmatic sulphide systems are dominantly
controlled by the dynamics and kinetics of transported sulphide liquid droplets. We examine …

Magmatic sulfide deposits are generated by extraordinary accumulations of immiscible
sulfide liquids in ultramafic-mafic magmas. While their associated geochemical and …

Much of the value of magmatic Ni-Cu-PGE sulfide orebodies is contained within massive or
semi-massive ores that show a wide variety of textural relationships to included or adjacent …