The aim of this study is to investigate the stable isotope composition of terrestrial mantle rocks (S, Te and Pd) and chondritic meteorites (Te and Pd) and to calibrate experimentally the stable isotope fractionation for the aforementioned elements imparted by metal-silicate equilibration during core formation. The measurements and experiments will constrain the geochemical behavior of S, Te, and Pd and their isotopes during core formation and may help to explain the observed isotopic differences between chondrites and bulk silicate Earth.
Fischer-Gödde, Mario | Professorship for experimental and analytical planetology (Prof. Kleine) |
Klemme, Stephan | Professur für Petrologie (Prof. Klemme) |
Fischer-Gödde, Mario | Professorship for experimental and analytical planetology (Prof. Kleine) |
Klemme, Stephan | Professur für Petrologie (Prof. Klemme) |
Hellmann, Jan | Professorship for experimental and analytical planetology (Prof. Kleine) |