Serpentinites are central to water (re) cycling in subduction zones and thus effect fluid-
mediated element transfer between the hydrosphere and the Earth's mantle and back into …

Subduction of serpentinite-hosted carbonate rocks formed during the oceanic stage in the
oceanic lithosphere (ophicalcite) or by metasomatism at the slab mantle-wedge interface …

Carbonation of oceanic lithosphere occurs widely during seawater alteration, and subducted
carbonated oceanic lithosphere may play a key role in carbon recycling in subduction …

Interactions between meteoric water and ultramafic rocks in the Oman Ophiolite generate
waters of variable physicochemical characteristics. The discharge of these waters forms …

Climate is regulated by the carbonate–silicate cycle in which slab outgassing of C into deep
fluids and volcanic degassing of CO 2 into the atmosphere are an important part. However …

Fluids released through the dehydration of serpentinite can be rich in Cl−, which enables the
significant mobility of Cr in subduction zones. However, the Cr isotope behavior …

The interplay between structural and metamorphic processes operating along the deep
plate interface in subduction zones remains elusive as much of the geologic record is …

We present a detailed study of the water geochemistry, mineralogy and textures in
serpentinization-related hyperalkaline springs in the Ronda peridotites. Ronda waters can …

Subducted serpentinites have the potential to control the exchange of volatile and redox
sensitive elements (eg, Fe, S, C, N) between the slab, the mantle wedge and the deep …

The melting behavior of subducted ophicarbonate is experimentally investigated under
conditions relevant for slabs at subarc depths (2.5–6 GPa and 650–1000° C). Hydrous …