Characteristics of ten of the world's metallogenic provinces hosting iron oxide Cu-Au (IOCG)
deposits have been critically assessed, including their geological and tectonothermal …

The Sossego iron oxide–copper–gold deposit in the Carajás Mineral Province comprises
two major orebodies, Sequeirinho and Sossego. Sodic alteration (albite–hematite) and …

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 …

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 …

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 …

Liberation of iron and potassium by widespread postmetamorphic albitization of country
rocks was one of the likely contributing processes in the formation of both barren and …

The Sossego iron oxide–copper–gold deposit (245 Mt@ 1.1% Cu, 0.28 g/t Au) in the
Carajás Mineral Province of Brazil consists of two major groups of orebodies (Pista …

Variations in the abundances of light stable isotopes, particularly those of hydrogen, boron,
carbon, oxygen and sulfur, were essential in developing mineralization models. The data …

Fe-oxide-Cu-Au deposits typically formed in continental arc and intracratonic tectonic
settings, predominantly in the Proterozoic, but also during the Phanerozoic. The lack of …

The behaviour of copper in hydrothermal waters and brines is poorly known at the pressure–
temperature–salinity conditions typical of magmatic-hydrothermal systems, severely limiting …