Ca and Mg isotope fractionation during the stoichiometric dissolution of dolomite at temperatures from 51 to 126 °C and 5 bars CO2 pressure

A. Perez-Fernandez, U. N. Berninger, V. Mavromatis, P. A.E. Pogge von Strandmann, E. H. Oelkers*

*Corresponding author for this work

Research output: Contribution to journal › Article › peer-review

Fingerprint

Dive into the research topics of 'Ca and Mg isotope fractionation during the stoichiometric dissolution of dolomite at temperatures from 51 to 126 °C and 5 bars CO2 pressure'. Together they form a unique fingerprint.

Earth and Planetary Sciences

Agricultural and Biological Sciences