EGU24-2357, updated on 08 Mar 2024
https://doi.org/10.5194/egusphere-egu24-2357
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under the Creative Commons Attribution 4.0 License.
Detrital zircon characteristics of Paleoproterozoic-Ordovician in the Olongbuluke Terrane: implication for the affinity of Olongbuluke Terrane and the closure of the Proto-Tethys Ocean
- Department of Geology, Northwest University , Geology, Xi'an, China (wuhn2506@nwu.edu.cn)
How to cite: Wang, T., Zhou, Y., and Wu, H.: Detrital zircon characteristics of Paleoproterozoic-Ordovician in the Olongbuluke Terrane: implication for the affinity of Olongbuluke Terrane and the closure of the Proto-Tethys Ocean, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-2357, https://doi.org/10.5194/egusphere-egu24-2357, 2024.