Renewed economic interest in iron oxide–apatite (IOA) deposits—containing tens to
hundreds of millions of tonnes of Fe and substantial amounts of rare earth elements, P, Co …

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 …

Apatites from the major types of mainly magmatic-hydrothermal mineral deposits (30
localities, mostly in British Columbia, Canada) together with apatites from carbonatites (29 …

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 …

The origin of iron oxide-apatite deposits is controversial. Silicate liquid immiscibility and
separation of an iron-rich melt has been invoked, but Fe–Ca–P-rich and Si-poor melts …

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 …

The ratio of the halogens F and Cl in apatite is highly sensitive to changes in the
composition of an evolving silicate melt or aqueous fluid. For this reason apatite chemistry is …

Abstract High-titanium (high-Ti, more than 1 wt% Ti) magnetite, commonly containing
ilmenite exsolution, has long been attributed to an igneous origin and has been used as the …

We propose an integrated model that explains the magmatic and hydrothermal features of
the unique El Laco iron deposit that is located in a Pliocene–Pleistocene volcano of the …

Magnetite-(apatite) ore deposits are interpreted as being formed by the crystallization of iron-
rich ultrabasic melts, dominantly generated by the interaction of silicate melts with oxidized …