[HTML][HTML] Fenites associated with carbonatite complexes: A review
Carbonatites and alkaline-silicate rocks are the most important sources of rare earth
elements (REE) and niobium (Nb), both of which are metals imperative to technological …
elements (REE) and niobium (Nb), both of which are metals imperative to technological …
Fluid and mass transfer at subduction interfaces—The field metamorphic record
GE Bebout, SC Penniston-Dorland - Lithos, 2016 - Elsevier
The interface between subducting oceanic slabs and the hanging wall is a structurally and
lithologically complex region. Chemically disparate lithologies (sedimentary, mafic and …
lithologically complex region. Chemically disparate lithologies (sedimentary, mafic and …
The chemistry of subduction-zone fluids
CE Manning - Earth and Planetary Science Letters, 2004 - Elsevier
Subduction zones generate voluminous magma and mediate global element cycling. Fluids
are essential to this activity, yet their behavior is perhaps the most poorly understood aspect …
are essential to this activity, yet their behavior is perhaps the most poorly understood aspect …
Metamorphic chemical geodynamics of subduction zones
GE Bebout - Earth and Planetary Science Letters, 2007 - Elsevier
Study of metamorphic suites directly representing the deep subduction of altered oceanic
crust and sediments can help elucidate the geochemical evolution of the forearc-to-subarc …
crust and sediments can help elucidate the geochemical evolution of the forearc-to-subarc …
Massive production of abiotic methane during subduction evidenced in metamorphosed ophicarbonates from the Italian Alps
A Vitale Brovarone, I Martinez, A Elmaleh… - Nature …, 2017 - nature.com
Alteration of ultramafic rocks plays a major role in the production of hydrocarbons and
organic compounds via abiotic processes on Earth and beyond and contributes to the …
organic compounds via abiotic processes on Earth and beyond and contributes to the …
Dehydration of subducting serpentinite: implications for halogen mobility in subduction zones and the deep halogen cycle
We investigated the halogen (Cl, F, Br, and I) chemistry of serpentinites that record
progressive dehydration during subduction from shallow oceanic environments via …
progressive dehydration during subduction from shallow oceanic environments via …
Trace-element mobilization in slabs due to non steady-state fluid–rock interaction: constraints from an eclogite-facies transport vein in blueschist (Tianshan, China)
The mafic high-pressure rocks of the Tianshan (NW China) display an interconnected
network of eclogite-facies veins derived by prograde blueschist dehydration. They provide …
network of eclogite-facies veins derived by prograde blueschist dehydration. They provide …
Trace element fractionation during fluid-induced eclogitization in a subducting slab: trace element and Lu–Hf–Sm–Nd isotope systematics
Spatially closely associated gabbros and eclogites of central Zambia represent relics of
subducted oceanic crust in a suture zone. The eclogites, which formed at 630–690° C and …
subducted oceanic crust in a suture zone. The eclogites, which formed at 630–690° C and …
Serpentinites of the Zermatt‐Saas ophiolite complex and their texture evolution
XP Li, M Rahn, K Bucher - Journal of Metamorphic Geology, 2004 - Wiley Online Library
Abstract The Zermatt‐Saas serpentinite complex is an integral member of the Penninic
ophiolites of the Central Alps and represents the mantle part of the oceanic lithosphere of …
ophiolites of the Central Alps and represents the mantle part of the oceanic lithosphere of …
Carbonation by fluid–rock interactions at high-pressure conditions: implications for carbon cycling in subduction zones
Carbonate-bearing lithologies are the main carbon carrier into subduction zones. Their
evolution during metamorphism largely controls the fate of carbon, regulating its fluxes …
evolution during metamorphism largely controls the fate of carbon, regulating its fluxes …