Porphyry deposits are large, low-grade metal ore bodies that are formed from hydrothermal
fluids derived from an underlying magma reservoir. They are important as major sources of …

Magmatic sulfide deposits are generated by extraordinary accumulations of immiscible
sulfide liquids in ultramafic-mafic magmas. While their associated geochemical and …

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

Magmatic systems play a crucial role in enriching the crust with volatiles and elements that
reside primarily within the Earth's mantle, including economically important metals like …

Much of the world's supply of battery metals and platinum group elements (PGE) comes from
sulphide ore bodies formed in ancient sub-volcanic magma plumbing systems. Research on …

The world‐class magmatic sulfide deposits in the Norilsk region exhibit a remarkable spatial
and temporal association with the Siberian large igneous province (LIP). However, the …

The Current deposit is hosted by serpentinized peridotite that intruded rocks of the Quetico
Subprovince in the Midcontinent Rift, and is subdivided into three morphologically distinct …

Efficient transfer of S and chalcophile metals through the Earth's crust in arc systems is
paramount for the formation of large magmatic-hydrothermal ore deposits. The formation of …

Arc basalts with high H 2 O content are expected to evolve into highly hydrated felsic melts
saturated with aqueous fluids at lower crustal pressures, which are potentially important in …

Loss of magmatic sulfides to the mantle is posited to explain the copper deficit of evolved arc
magmas and the depleted Cu/Ag ratio of the continental crust. We address the question of …