EGU25-1610, updated on 14 Mar 2025
https://doi.org/10.5194/egusphere-egu25-1610
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Evaluation of the role of detachment faulting in the genesis of felsic melts in the Atlantis Bank oceanic core complex, Southwest Indian Ridge
Wei-Qi Zhang1,3, Chuan-Zhou Liu2,3,4, Christopher J MacLeod5, and C. Johan Lissenberg5
Wei-Qi Zhang et al.
  • 1Key Laboratory of Submarine Geosciences, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou, China
  • 2Laoshan Laboratory, Qingdao, China
  • 3State Key Laboratory of Lithospheric and Environmental Coevolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China
  • 4University of Chinese Academy of Sciences, Beijing, China
  • 5School of Earth and Ocean Sciences, Cardiff University, Cardiff, UK

How to cite: Zhang, W.-Q., Liu, C.-Z., MacLeod, C. J., and Lissenberg, C. J.: Evaluation of the role of detachment faulting in the genesis of felsic melts in the Atlantis Bank oceanic core complex, Southwest Indian Ridge, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-1610, https://doi.org/10.5194/egusphere-egu25-1610, 2025.

This abstract has been withdrawn on 25 Jul 2025.