Zn and Fe isotopes indicate that kimberlites and silica-undersaturated magmas derive from similar asthenospheric mantle sources

Authors

  • Ronghua Cai
  • Andrea Giuliani
  • Paolo A. Sossi
  • Tian-Hao Wu
  • Yongsheng He
  • Sheng-Ao Liu
  • D. Graham Pearson
  • Jingao Liu

DOI:

https://doi.org/10.29173/ikc4071

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12th International Kimberlite Conference.

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Published

2024-07-08

How to Cite

Cai, R., Giuliani, A., Sossi, P. A., Wu, T.-H., He, Y., Liu, S.-A., … Liu, J. (2024). Zn and Fe isotopes indicate that kimberlites and silica-undersaturated magmas derive from similar asthenospheric mantle sources. International Kimberlite Conference: Extended Abstracts, 12. https://doi.org/10.29173/ikc4071

Issue

Vol. 12 (2024): Vol 12: International Kimberlite Conference, Yellowknife

Section

Extended Abstracts

License

Copyright (c) 2024 Author(s)

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This work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.

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