EGU26-9064, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-9064
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
Multiple mantle metasomatism scenarios in Kempirsai ophiolite, Kazakhstan: Evidence from the borehole peridotites
1,2,3,2,- 1Tianjin Geological Survey Center, China Geological Survey, Tianjin, China
- 2Chair of Geology and Economic Geology, Montanuniversität Leoben, Leoben, Austria
- 3Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China
- 4State Key Laboratory of Lithospheric and Environmental Coevolution, Institute of Geology and Geophysics, Chinese Academy of Science, Beijing, China
- 5University of Chinese Academy of Sciences, Beijing, China
- 6Institut für Erdsystemwissenschaften, Leibniz University Hannover, Callinstrasse 3, Hannover, Germany
How to cite: Liu, X., Melcher, F., Xiao, Y., Su, B.-X., Erlandsson, V. B., and Merseburger, S.: Multiple mantle metasomatism scenarios in Kempirsai ophiolite, Kazakhstan: Evidence from the borehole peridotites, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-9064, https://doi.org/10.5194/egusphere-egu26-9064, 2026.