Mineral deposits represent extraordinary metal concentrations that form by magmatic,
magmatic–hydrothermal or hydrothermal processes in geodynamic environments typified by …

Tectono-metallogenic systems are geological systems that link geodynamic and tectonic
processes with ore-forming processes. Fundamental geodynamic processes, including …

The iron oxide copper-gold (IOCG) group of deposits, initially defined following discovery of
the giant Olympic Dam Cu-U-Au deposit, has progressively become too-embracing when …

Many diverse ore systems are classified together as iron oxide copper-gold (IOCG) deposits
based on an empirical definition arising primarily from geochemical features that do not …

Iron oxide-copper-gold (IOCG) deposits, defined primarily by their elevated magnetite and/or
hematite contents, constitute a broad, ill-defined clan related to a variety of tectono …

The Andes, in particular their central parts, have been known as a preeminent Cu province
for more than 100 years and have been the source of many innovative metallogenic …

Several iron oxide-rich Cu-Au (-Zn-Ag) deposits define an approximately 5-km-wide and at
least 20-km-long belt along the eastern margin of the coastal batholith near Copiapó, Chile …

Pyrite is ubiquitous in the world-class iron oxide copper-gold (IOCG) deposits of the
Candelaria-Punta del Cobre district, documented from early to late stages of mineralization …

The eastern Gawler craton hosts Australia's premier uranium-bearing iron oxide copper-gold
(IOCG) belt, the> 500-km-long Olympic Cu-Au-(U) province. In addition to the Olympic Dam …

Abstract Major Cu–Au deposits of iron oxide–copper–gold (IOCG) style are temporally
associated with oxidized, potassic granitoids similar to those linked to major porphyry Cu …