Zn isotope fractionation during adsorption to calcite and birnessite surfaces, and the aim is to understand why marine carbonates and ferromanganese crusts are enriched in heavy isotopes of Zn relative to average seawater
Zn isotope fractionation during adsorption to calcite and birnessite surfaces, and the aim is to understand why marine carbonates and ferromanganese crusts are enriched in heavy isotopes of Zn relative to average seawater