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)
DOI:
https://doi.org/10.29173/ikc3501Downloads
Download data is not yet available.
Downloads
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
Issue
Section
Extended Abstracts