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 …

Iron oxide–apatite (IOA) and skarn Fe deposits are important sources of Fe in China. During
the Mesozoic, a large number of large IOA and skarn Fe deposits formed in the Middle …

Kiruna-type iron oxide–apatite (IOA) deposits, an important source of iron, show close
associations with andesitic subvolcanic intrusions. However, the processes of ore formation …

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 …

Magnetite-apatite deposits are important sources of iron and other metals. A prominent
example are the magnetite lavas at the El Laco volcano, Northern Chile. Their formation …

The generation of sulfate-rich hydrothermal fluids is of great significance to investigate
because it is closely associated with the formation of many important ore deposits, such as …

The origin of magnetite-(apatite) iron deposits (MtAp) is one of the most contentious issues
in ore geology with competing models that range from hydrothermal to magmatic processes …

Magnetite is the main constituent of iron oxide–apatite (IOA) deposits, which are a globally
important source of Fe and other elements such as P and REE, critical for modern …

Chemical exchange between silicate magmas and carbonate rocks has major implications
for igneous fractionation, atmospheric CO2 flux, and formation of mineral deposits. However …

The long-standing controversy about the origin of magnetite-(apatite) mineral deposits
pertains to how they form. The Pleistocene El Laco deposit in northern Chile is a critical …