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Publikationen

The effect of COH fluids on partial melting of eclogite and lherzolite under moderately oxidizing and reducing conditions Liu, Z; Rohrbach, A; Tiraboschi, C; Foley, SF; Berndt, J; Klemme, S (2023) In: Chemical Geology, 121219. Forschungsartikel (Zeitschrift)
Preferential mobilisation of oxidised iron by slab-derived hydrous silicate melts Tiraboschi, C; McCammon, C; Rohrbach, A; Klemme, S; Berndt, J; Sanchez-Valle, C (2023) In: Geochemical Perspectives Letters, 24. Forschungsartikel (Zeitschrift)
Iron mobility in slab-derived hydrous silicate melts at sub-arc conditions Tiraboschi C, Rohrbach A, Klemme S, Berndt J, Sanchez-Valle C (2022) In: (Hrsg.), . (kein Verlag angegeben). Forschungsartikel in Sammelband (Konferenz)
The stability of antigorite in subduction zones revisited: The effect of F on antigorite stability and its breakdown reactions at high pressures and high temperatures, with implications for the geochemical cycles of halogens Flemetakis, S; Tiraboschi, C; Rohrbach, A; Berndt, J; Klemme, S (2022) In: Contributions to Mineralogy and Petrology, 177. Forschungsartikel (Zeitschrift)
Carbon-saturated COH fluids in the upper mantle: a review of high-pressure and high-temperature ex situ experiments Tiraboschi, C; Miozzi, F; Tumiati, S (2022) In: European Journal of Mineralogy, 34. Forschungsartikel (Zeitschrift)
Subducted organic matter buffered by marine carbonate rules the carbon isotopic signature of arc emissions. Tumiati, S; Recchia, S; Remusat, L; Tiraboschi, C; Sverjensky, D; Manning, CE; Vitale-Brovarone, A; Boutier, A; Spanu, D; Poli, S (2022) In: Nature Communications, 13.
An Experimental Study on Kinetics-Controlled Ca-Carbonate Aqueous Reduction into CH4 (1 and 2 GPa, 550°C): Implications for C Mobility in Subduction Zones In: .
Dissolution susceptibility of glass-like carbon versus crystalline graphite in high-pressure aqueous fluids and implications for the behavior of organic matter in subduction zones. In: .
Experimental determination of magnesia and silica solubilities in graphite-saturated and redox-buffered high-pressure COH fluids in equilibrium with forsterite + enstatite and magnesite + enstatite. In: .
Silicate dissolution boosts the CO2 concentration in subduction fluids. In: .