Although the term orogenic gold has become widely accepted over the past 20 years for
disseminated-to lode-style gold deposits that formed in a variety of tectonic environments …

In most published hydrothermal ore deposit models, the main agent of metal transport is an
aqueous liquid. However, there is increasing evidence from volcanic vapors, geothermal …

A metamorphic devolatilization model can explain the enrichment, segregation, timing,
distribution and character of many goldfields such as those found in Archean greenstone …

Although gold is a noble metal and is effectively insoluble even in strong acids, we have
known for nearly 500 years that it can be concentrated to mineable levels by being …

Fluid-phase relationships and thermodynamic reaction modelling based on published
mineral solubility data are used to re-assess the Cu–Au-mineralising fluid processes related …

The hydration and complexation of metals in hydrothermal fluids are key processes
controlling the mobility of elements in the Earth's crust, leading to the formation of ore …

Metal-rich fluids that circulate in magmatic-hydrothermal environments form a wide array of
economically significant ore deposits. Unravelling the origins and evolution of these fluids is …

Economically exploitable deposits of metallic minerals (ore deposits) form in the Earth's crust
through a variety of geologic processes. These involve extraction of metals at low …

Extensive research during the 20 th century on porphyry Cu (-Mo-Au) deposits has revealed
the following major geodynamic, petrological, mineralogical, and geochemical features that …

Fluid-phase stability relations combined with thermodynamic modeling using fluid-inclusion
analyses and new gold-solubility experiments lead to an integrated geological interpretation …