Peridotitic diamond formation at Panda (Slave craton, Canada) from paleo-subduction wedge- or mantle-derived fluids ? The bearing of stable isotope data (15N/14N, 33S/32S, 34S/32S, /12C)

Authors

  • P. Cartigny
  • J. Farquhar
  • J.W. Harris
  • B. Wing
  • A. Masterson
  • K. McKeegan
  • T.S. Stachel

DOI:

https://doi.org/10.29173/ikc3501

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Published

2008-10-15

How to Cite

Cartigny, P., Farquhar, J., Harris, J., Wing, B., Masterson, A., McKeegan, K., & Stachel, T. (2008). Peridotitic diamond formation at Panda (Slave craton, Canada) from paleo-subduction wedge- or mantle-derived fluids ? The bearing of stable isotope data (15N/14N, 33S/32S, 34S/32S, /12C). International Kimberlite Conference: Extended Abstracts, 9. https://doi.org/10.29173/ikc3501

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