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Subducted carbon weakens the forearc mantle wedge in a warm subduction zone
Subducting oceanic plates carry large amounts of carbon into the Earth's interior. The
subducted carbon is mobilized by fluid and encounters ultramafic rocks in the mantle wedge …
subducted carbon is mobilized by fluid and encounters ultramafic rocks in the mantle wedge …
Carbonation processes in Oman peridotite: temperature-dependent reactions and Mg isotope composition of reacting fluids
The study of natural analogues of CO 2 mineral sequestration combined with the
experimental quantification of carbonation reactions constitutes a fundamental approach to …
experimental quantification of carbonation reactions constitutes a fundamental approach to …
Experimental evidence for reaction‐induced weakening of (carbonated) serpentinite fault gouges
The seismic potential of faults depends on the local mineralogy and can change upon
mineral reactions. We conducted friction experiments on serpentinite, carbonate and …
mineral reactions. We conducted friction experiments on serpentinite, carbonate and …
Integration of mineralogical, geochemical and ASD reflectance spectra data for characterization and evolution of Neoproterozoic serpentinites and listwaenites at …
AA Surour, AA Madani, MA El Sobky - Geochemistry, 2025 - Elsevier
The present research focuses on the application some remote sensing techniques, mostly
ASD FeldSpec combined with principal component analysis (PCA) and fusion color …
ASD FeldSpec combined with principal component analysis (PCA) and fusion color …
[HTML][HTML] Mineralogy and Geochemistry of Listvenite-Hosted Ni–Fe Sulfide Paragenesis—A Case Study from Janjevo and Melenica Listvenite Occurrences (Kosovo)
The main goal of this paper is to determine the order of the paragenetic sequence and
phase transitions of the Ni–Fe sulfide association hosted in listvenites. Listvenites are …
phase transitions of the Ni–Fe sulfide association hosted in listvenites. Listvenites are …
Fluid-rock interactions and sulphur mobility during carbonation of the Point-Rousse ophiolite complex: implications for carbon and sulphur cycling in forearc settings
ID Garduño-Torres, MD Menzel, JA Padrón-Navarta… - 2025 - digital.csic.es
The interaction of CO2-bearing fluids with hydrated mafic and ultramafic rocks results in the
replacement of minerals such as serpentine and brucite by dolomite and magnesite. This …
replacement of minerals such as serpentine and brucite by dolomite and magnesite. This …