Volatile elements (water, carbon, nitrogen, sulfur, halogens, and noble gases) played an
essential role in the secular evolution of the solid Earth and emergence of life. Here we …

We have compiled the trace element concentrations in pyrrhotite, pentlandite, chalcopyrite,
and pyrite from magmatic Ni-Cu-PGE ore deposits with the aim of understanding their …

The platinum-group minerals (PGM) are a diverse group of minerals that concentrate the
platinum-group elements (PGE; Os, Ir, Ru, Rh, Pt, and Pd). At the time of writing, the …

Magmatic Ni–sulfide ore deposits are generally associated with basaltic to komatiitic
igneous rocks that originate by partial melting of the mantle, which is usually modelled as a …

Abyssal peridotites are oceanic mantle fragments that were recently processed through
ridges and represent residues of both modern and ancient melting. To constrain the nature …

Diamond crystallization ages are essential information for science and industry, leading to
an understanding of how, why, and where diamonds form in Earth and how best to find …

Addition of crustal sulfur to the **chuan magma or oxidation of the magma associated with
carbonate assimilation has been considered to be the main cause of sulfide saturation in the …

In whole-Earth models of volatile cycles the outflux from our planet's convecting mantle to its
surface via volcanoes, including those essential for life (eg C, H 2 O, S, F, Cl), is traditionally …

Cratonic lithospheric mantle is composed of predominantly refractory materials that formed
at higher mantle potential temperatures (TP) than recorded in non-cratonic peridotites. It also …

The ultramafic mantle sections of the Yarlung-Zangbo ophiolites (YZO) along the suture of
India and Asia in Tibet preserve the mantle history of the formerly intervening oceanic …