GFZ German research centre for geo sciences

Formation of rare-metal (Li, Be, Sn, W) deposits and the Rumsveld matrix: From unknown knowns and known unknowns to known knowns

Liu, Y., Schmidt, C., Li, J., Wang, D., Yan, Q., Stammeier, J. A., Sieber, M. J. (2024): The role of protolith composition in the formation of tin-enriched granitic melts: A modeling study using the example of the southwest China tin province. - Ore Geology Reviews, 169, 106094. https://doi.org/10.1016/j.oregeorev.2024.106094

Romer, R. L., Kroner, U., Schmidt, C., Legler, C. (2022): Mobilization of tin during continental subduction-accretion processes. - Geology, 50, 12, 1361-1365. https://doi.org/10.1130/G50466.1

Liu, Y., Schmidt, C., Li, J. (2022): Peralkalinity in peraluminous granitic pegmatites. I. Evidence from whewellite and hydrogen carbonate in fluid inclusions. - American Mineralogist, 107, 2, 233-238. https://doi.org/10.2138/am-2021-7790

Liu, Y., Schmidt, C., Li, J. (2022): Peralkalinity in peraluminous granitic pegmatites. II. Evidence from experiments on carbonate formation in spodumene-bearing assemblages. - American Mineralogist, 107, 2, 239-247. https://doi.org/10.2138/am-2021-7909

Schmidt, C., Gottschalk, M., Zhang, R., Lu, J. (2021): Oxygen fugacity during tin ore deposition from primary fluid inclusions in cassiterite. - Ore Geology Reviews, 139, Part A, 104451.
https://doi.org/10.1016/j.oregeorev.2021.104451

Schmidt, C., Romer, R. L., Wohlgemuth-Ueberwasser, C., Appelt, O. (2020): Partitioning of Sn and W between granitic melt and aqueous fluid. - Ore Geology Reviews, 117, 103263. https://doi.org/10.1016/j.oregeorev.2019.103263

Schmidt, C. (2018): Formation of hydrothermal tin deposits: Raman spectroscopic evidence for an important role of aqueous Sn(IV) species. - Geochimica et Cosmochimica Acta, 220, 499-511. https://doi.org/10.1016/j.gca.2017.10.011

Partner

Dr. Melanie Sieber, Universität Potsdam, Institut für Geowissenschaften

Rongqing Zhang, Nanjing University, Nanjing, China

Yongchao Liu, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing, China

back to top of main content