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 …

Abstract Magmatic Ni-Cu-PGE sulfide assemblages are almost ubiquitously comprised of
pyrrhotite-pentlandite-chalcopyrite (-pyrite). Sulfide alteration is common during syn-or post …

Abstract The porphyry Cu-Mo deposit in Butte, Montana, formed where magmatic
hydrothermal fluids, introduced with injections of porphyrytic dikes, fractured and permeated …

Abstract The Yulong porphyry Cu (Au) deposit occurs on the eastern margin of the Tibetan
plateau and is one of the largest porphyry Cu (Au) deposits in China, containing more than 6 …

Magmatic arcs are terrestrial environments where lithospheric cycling and recycling of
metals and volatiles is enhanced. However, the first-order mechanism permitting the …

Abstract The Xiarihamu Ni-Co deposit, located in the East Kunlun orogenic belt, northern
Tibet plateau, is the secondary largest Ni deposit in China and contains~ 157 million metric …

Sulfur and chlorine are the two most important ligands accounting for metal transport in the
upper crust. In this study, four metal-and sulfur-saturated model fluids with varying salinities …

Abstract The Mid-Cayman spreading centre is an ultraslow-spreading ridge in the
Caribbean Sea. Its extreme depth and geographic isolation from other mid-ocean ridges …

Scavenging of gold during metamorphic devolatilization is a widely accepted model for fluid
and metal sourcing in orogenic gold deposits. In order to further constrain this process and …

Thermochronology finds many applications in economic geology. Utilizing
temperaturesensitive radiometric dating techniques to reveal low-temperature, upper crustal …