The solubilities of chloride (Cl−) and H2O in aluminosilicate melts of basalt, andesite, and
latite compositions saturated in aqueous vapor and/or hydrosaline liquid were determined at …

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 …

This contribution provides an overview of available experimental, thermodynamic, and
molecular data on Au aqueous speciation, solubility, and partitioning in major types of …

Abstract Magmatic Fe-Ni-Cu±platinum-group element (PGE) sulfide deposits form when
mantle-derived mafic and ultramafic magmas become saturated in sulfide and segregate …

Veined peridotite xenoliths from the mantle beneath the giant Ladolam gold deposit on Lihir
Island, Papua New Guinea, are 2 to 800 times more enriched in copper, gold, platinum, and …

THE source of the hydrothermal fluids vented in active volcanic areas on the sea floor1–3
has been a matter of some debate4–7; they may arise purely from the interaction of …

The concentrations of the platinum-group elements (PGE) Ir, Ru, Pt, and Pd were
determined in 18 mantle-derived basalts from a variety of tectonic settings and six komatiites …

Compatible behaviour has been considered as a major influence on the behaviour of the
platinum-group elements (PGE) in magmatic systems. The authors believe that current …

The platinum-group elements (PGEs; Os, Ir, Ru, Rh, Pt, Pd), along with rhenium and gold,
are grouped together as the highly siderophile elements (HSEs), defined by their extreme …

Concentration patterns of platinum-group elements (PGE) in the Lower, Critical and Main
Zones of the Bushveld Complex are modelled by a process of metal collection by …