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Complexity of graphite formation in response to metamorphic methane generation and transformation in an orogenic ultramafic body
The fate of carbon in subduction is explored by considering fluid-rock interactions in a body
of metamorphosed ultramafic rocks from the Appalachian belt as potential proxies for …
of metamorphosed ultramafic rocks from the Appalachian belt as potential proxies for …
Formation of hydrocarbons favored by high pressure at subduction zone conditions
Subduction zones enable carbon transport to the deep Earth. Inorganic and organic carbon
in fluids released from the subducted slab are important in water-rock interactions. However …
in fluids released from the subducted slab are important in water-rock interactions. However …
Coupled cycling of carbon and water in the form of hydrous carbonatitic liquids in the subarc region
W Chen, S Keshav, W Peng… - Journal of Geophysical …, 2023 - Wiley Online Library
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 …
conditions relevant for slabs at subarc depths (2.5–6 GPa and 650–1000° C). Hydrous …
Experimental dissolution of carbonaceous materials in water at 1 GPa and 550° C: Assessing the role of carbon forms and redox state on COH fluid production and …
Biogenic carbonaceous material (CM) is the main carrier of organic carbon in the subduction
zone and contributes to COH fluid production and volcanic arc gaseous emissions. Here we …
zone and contributes to COH fluid production and volcanic arc gaseous emissions. Here we …
Immiscible metamorphic water and methane fluids preserved in carbonated eclogite
Subduction zones metamorphic fluids are pivotal in geological events such as volcanic
eruptions, seismic activity, mineralization, and the deep carbon cycle. However, the …
eruptions, seismic activity, mineralization, and the deep carbon cycle. However, the …
A reliable analytical procedure to determine the carbon isotopic signature of CO2-bearing COH fluids generated in petrological experiments
L Toffolo, L Minopoli, E Ferrari… - European Journal of …, 2025 - ejm.copernicus.org
The ratio of stable carbon isotopes, δ 13 C, serves as a fundamental tracer for geological
processes. Experiments aiming to replicate isotopic exchange between carbon reservoirs …
processes. Experiments aiming to replicate isotopic exchange between carbon reservoirs …