EGU26-17017, updated on 20 Apr 2026
https://doi.org/10.5194/egusphere-egu26-17017
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
Mercury isotopic turnover in 2.6–2.5 Ga granitoids: Evidence of oceanic subduction on late Neoarchean Earth
- University of Hong Kong, Department of Earth and Planetary Sciences, Hong Kong, Hong Kong (changrh@hku.hk)
How to cite: Chang, R.: Mercury isotopic turnover in 2.6–2.5 Ga granitoids: Evidence of oceanic subduction on late Neoarchean Earth, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-17017, https://doi.org/10.5194/egusphere-egu26-17017, 2026.