Sulfide trace element signatures as a tracer for low- and high-temperature processes in serpentinites

Malte Kalter; Esther M. Schwarzenbach; Falco Menne; Marcus Oelze; Martin J. Whitehouse; Timm John

doi:https://doi.org/10.5194/egusphere-egu22-8070

[Back] [Session TS1.2]

EGU22-8070, updated on 28 Mar 2022

https://doi.org/10.5194/egusphere-egu22-8070

EGU General Assembly 2022

© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

Sulfide trace element signatures as a tracer for low- and high-temperature processes in serpentinites

Malte Kalter¹, Esther M. Schwarzenbach¹, Falco Menne¹, Marcus Oelze^2,3, Martin J. Whitehouse⁴, and Timm John¹

Malte Kalter et al.

¹Freie Universität Berlin, Institute of Geological Science, Berlin, Germany
²GFZ German Research Centre for Geosciences, Potsdam, Germany
³Present address: BAM Bundesanstalt für Materialprüfung und -forschung, Berlin, Germany
⁴Department of Geosciences, Swedish Museum of Natural History, 104 05 Stockholm, Sweden

How to cite: Kalter, M., Schwarzenbach, E. M., Menne, F., Oelze, M., Whitehouse, M. J., and John, T.: Sulfide trace element signatures as a tracer for low- and high-temperature processes in serpentinites, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-8070, https://doi.org/10.5194/egusphere-egu22-8070, 2022.

This abstract has been withdrawn on 20 May 2022.