Layered mafic intrusions are significant sources of the platinum-group elements, base metal
sulphides, chromite, magnetite, and ilmenite. The distribution of these ores is reviewed, with …

Several correlation methods are used to estimate data and equation-of-state parameters that
permit calculation of standard state thermodynamic properties at high pressures and …

Magmatic sulfide deposits consist of pyrrhotite, pentlandite, chalcopyrite (±pyrite), and
platinum-group minerals (PGM). Understanding the distribution of the chalcophile and …

The platinum-group element (PGE) contents of the upper portions of the Bushveld Complex
were investigated with three questions in mind:(a) In natural systems does magnetite …

Mafic and ultramafic intrusions in the Pan-Xi area along the western margin of the Yangtze
block, southwestern China, are spatially associated with the Late Permian Emeishan flood …

Orogenic lherzolites exhibit a specific (although reproducible) platinum-group element
signature characterized by slight positive deviations of Pd/Ir, Rh/Ir and Ru/Ir ratios from the …

The Keivitsansarvi deposit, in northern Finland, is a low-grade dissemination of Ni–Cu
sulfides containing 1.3–26.6 g/t PGE. It occurs in the northeastern part of the 2.05 Ga …

Summary¶ We report, for the first time, the occurrence of five palladium-rich, one palladium
bearing and two gold-silver minerals from podiform chromitites in the Eastern Alps. Minerals …

ABSTRACT The Aguablanca Ni–Cu–PGE ore deposit, in southwestern Iberia, has a
magmatic origin, and has been reworked by later skarn-related hydrothermal activity. Base …

Abstract The Main Sulfide Zone (MSZ) is the most prominent layer of the Great Dyke layered
intrusion carrying economic platinum-group element (PGE) mineralization. At the Hartley …