The continental crust is strongly depleted in copper compared with its building blocks—
primary arc magmas—and this depletion is intrinsically associated with continental crust …

The genesis of giant gold provinces is an international scientific frontier, in which the source
of a huge amount of gold and the drive for mineralization are key challenges. The …

Oxidation of the sub-arc mantle driven by slab-derived fluids has been hypothesized to
contribute to the formation of gold deposits in magmatic arc environments that host the …

The subduction-related Saindak porphyry Cu-Au deposit lies in the western segment of the
Chagai belt, Pakistan. This deposit consists of three orebodies (south, east, and north), and …

The transfer of chalcophile metals across the continental lithosphere has been traditionally
modeled based on their chemical equilibrium partitioning in sulfide liquids and silicate …

Abstract The Jiguanzui-Taohuazui Cu-Au deposit is located in the Edong ore district, Middle–
Lower Yangtze River metallogenic belt, eastern China. The deposit is palladium, platinum …

Abstract Porphyry Cu–Au deposits are the major global source of copper, an essential metal
for the green transition, and a significant source of gold. They occur both in thick continental …

Investigation of Hg isotope ratios of gold-related sulfides and penecontemporaneous mafic
dikes from four orogenic gold provinces on the margins of the North China Craton and …

Exposures of the Earth's crust-mantle transition are scarce, thus, limiting our knowledge
about the formation of subcontinental underplate cumulates, and their significance for metal …

A magnetotelluric (MT) study across the Red Lake greenstone belt of the western Superior
craton, Canada, images a 50-km-long north-dipping conductor (< 20 Ω· m) at 20–25 km …