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 …

Metals such as Cu, Mo, Au, Sn, and W in porphyry and related epithermal mineral deposits
are derived predominantly from the associated magmas, via magmatic–hydrothermal fluids …

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 …

Porphyry copper deposits are currently the world's largest source of copper and
molybdenum, and are also among the largest reservoirs of gold in the upper crust. Despite …

Hydrothermal pyrite contains significant amounts of minor and trace elements including As,
Pb, Sb, Bi, Cu, Co, Ni, Zn, Au, Ag, Se and Te, which can be incorporated into nanoparticles …

Determining the association of Pb–Zn (-Ag) mineralization with granite is crucial for
understanding metallogeny and identifying exploration targets. The genesis of Pb–Zn-Ag-Sb …

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 …

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 …

Processes responsible for high-grade gold enrichment are of significant economic interest
and have long been elusive. Structural and geophysical models postulate that earthquake …