Pyrite is one of the most common minerals in many precious and base metal hydrothermal
ore deposits and is an important host to a range of trace elements including Au and Co and …

Submarine hydrothermal sulfide ores occur at mid-ocean ridges, intra-oceanic arcs and in
back-arc basins associated with host rocks of highly variable composition. Pyrite is the …

The ubiquity of Au-bearing arsenian pyrite in hydrothermal ore deposits suggests that the
coupled geochemical behaviour of Au and As in this sulfide occurs under a wide range of …

The chemical composition, textures and mineral associations of pyrite provide key
information that help elucidate the evolution of hydrothermal systems. However, linking the …

Iron oxide-apatite (IOA) deposits are an important source of iron and other elements (eg,
REE, P, U, Ag and Co) vital to modern society. However, their formation, including the …

Trace elements in pyrite are increasingly being used in ore deposit exploration as a
geochemical pathfinder to ore. This is because the trace element systematics of pyrite are …

Textural and chemical characterization of pyrite was used to reconstruct the hydrothermal
evolution of the Bracemac-McLeod Archean volcanogenic massive sulfide (VMS) deposits …

Although studies have proposed that iron oxide-apatite (IOA) deposits may represent the
deeper roots of some Andean iron oxide copper-gold (IOCG) systems, their genetic links …

Porphyry deposits host various trace elements in economic amounts, but the hydrothermal
processes causing their fractionation and enrichment are still not fully understood, but vital to …

Abstract The Archaean Yilgarn Craton (Western Australia) is a world-class metallogenic
province, hosting considerable resources of Au, Ag, Ni, Cu, Zn and Fe. Here we present …