Water within the oceanic lithosphere is returned to Earth's surface at subduction zones. Observations of metamorphosed veins preserved in exhumed slabs suggest that fluid can …
The key role of serpentinites in the global cycles of volatiles, halogens and fluid-mobile elements in oceans and in subduction zones is now ascertained by many studies …
We investigated the halogen (Cl, F, Br, and I) chemistry of serpentinites that record progressive dehydration during subduction from shallow oceanic environments via …
We use the concentrations and isotope compositions of water, carbon, and sulfur in serpentinites and their dehydration products to trace the cycling of volatiles during …
The thermal structure of subduction zones is fundamental to our understanding of physical and chemical processes that occur at active convergent plate margins. These include …
The antigorite dehydration front preserved in the Cerro del Almirez (Nevado–Filábride Complex, Betic Cordillera, SE Spain) offers a unique opportunity to investigate the high …
Abstract Halogens (Cl, F, I, Br) are enriched in surface reservoirs compared to the mantle. The subduction of these reservoirs in the form of sedimentary pore fluids, sediments, altered …
B Debret, N Bolfan-Casanova… - … to Mineralogy and …, 2015 - Springer
Abstract The Cerro del Almirez massif (Spain) represents a unique fragment of serpentinized oceanic lithosphere that has been first equilibrated in the antigorite stability field (Atg …
S Angiboust, S Wolf, E Burov, P Agard… - Earth and Planetary …, 2012 - Elsevier
Both geophysical and petrological data suggest that large amounts of water are released in subduction zones during the burial of oceanic lithosphere through metamorphic dehydration …