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Perez-Fernandez, A.; Berninger, U.-N.; Mavromatis, V.; Pogge von Strandmann, P.A.E.; Oelkers, E.H. (2017). Ca and Mg isotope fractionation during the stoichiometric dissolution of dolomite at temperatures from 51 to 126 °C and 5 bars CO2 pressure. Chemical geology, 467, pp. 76-88. Elsevier 10.1016/j.chemgeo.2017.07.026
Critelli, T.; Marini, L.; Schott, J.; Mavromatis, V.; Apollaro, C.; Rinder, T.; De Rosa, R.; Oelkers, E.H. (2015). Dissolution rate of antigorite from a whole-rock experimental study of serpentinite dissolution from 2<pH<9 at 25°C: Implications for carbon mitigation via enhanced serpentinite weathering. Applied geochemistry, 61, pp. 259-271. Elsevier 10.1016/j.apgeochem.2015.06.004
Critelli, T.; Marini, L.; Schott, J.; Mavromatis, V.; Apollaro, C.; Rinder, T.; De Rosa, R.; Oelkers, E.H. (2014). Dissolution rates of actinolite and chlorite from a whole-rock experimental study of metabasalt dissolution from 2 ≤ pH ≤ 12 at 25 °C. Chemical geology, 390, pp. 100-108. Elsevier 10.1016/j.chemgeo.2014.10.013
Shirokova, L. S.; Mavromatis, V.; Bundeleva, I.; Pokrovsky, O.S.; Bénézeth, P.; Pearce, C.; Gérard, E.; Balor, S.; Oelkers, E.H. (2011). Can Mg isotopes be used to trace cyanobacteria-mediated magnesium carbonate precipitation in alkaline lakes? Biogeosciences Discussions, 8, pp. 6473-6517. Copernicus 10.5194/bgd-8-6473-2011
