The transport of water from subducting crust into the mantle is mainly dictated by the stability
of hydrous minerals in subduction zones. The thermal structure of subduction zones is a key …

The geochemical signatures of subducting crust have been identified in various types of
mafic igneous rocks at convergent plate boundaries, where island arc basalts (IAB) and …

Crustal recycling at convergent plate boundaries is essential to mantle heterogeneity.
However, crustal signatures in the mantle source of basaltic rocks above subduction zones …

Much of the present-day volume of Earth's continental crust had formed by the end of the
Archean Eon, 2.5 billion years ago, through the conversion of basaltic (mafic) crust into sodic …

The dynamics and evolution of Venus' mantle are of first-order relevance for the origin and
modification of the tectonic and volcanic structures we observe on Venus today. Solid-state …

Arc magmas globally are H2O-Cl-S–rich and moderately oxidized (ΔFMQ=+ 1 to+ 2) relative
to most other mantle-derived magmas (ΔFMQ≤ 0). Their relatively high oxidation state limits …

Continental basalts generally display enrichment of fluid-mobile elements and depletion of
high-field-strength elements, similar to those that evolved in the subduction environment, but …

Condensation contributes to soiling of photovoltaic modules by trap** dust particles and,
in certain conditions, leaving a material bridge between particles and the surface after …

For over 50 years, the use of high-pressure piston/cylinder apparatus combined with an
increasing diversity of microbeam analytical techniques has enabled the study of mantle …

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 …