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 …

Imaging rocks in three-dimensions through X-ray microtomography enables routine
visualization of structures in samples, which can be spatially resolved down to the sub …

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 …

Platinum-group element (PGE) deposits in the Bushveld Complex and other layered
intrusions form when large, incompletely solidified magma chambers undergo central …

We have compiled the trace element concentrations in pyrrhotite, pentlandite, chalcopyrite,
and pyrite from magmatic Ni-Cu-PGE ore deposits with the aim of understanding their …

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 …

Abstract The **arihamu Ni-Co deposit, located in the East Kunlun orogenic belt, northern
Tibet plateau, is the secondary largest Ni deposit in China and contains~ 157 million metric …

A large data compilation has been assembled of platinum group element (PGE) analyses in
mantle melts and mantle rocks, the latter including an assortment of xenoliths and obducted …

In the present paper, we have compiled data on 565 layered and differentiated igneous
intrusions globally, documenting their (i) location,(ii) age,(iii) size,(iv) geotectonic setting,(v) …

Equilibration between sulfide liquid and olivine is expressed in terms of the exchange
coefficient for Fe and Ni, KD=(XNiS/XFeS) sulfide_liquid/(XNiO/XFeO) olivine. The positive …