Geochemical processes in peridotite xenoliths from the Premier diamond mine, South Africa: evidence for depletion and refertilisation of subcratonic lithosphere

Authors

K.S. Viljoen
I.T.M. Dobbe
A.J. Smit

DOI:

https://doi.org/10.29173/ikc3356

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Published

2008-10-15

How to Cite

Viljoen, K., Dobbe, I., & Smit, A. (2008). Geochemical processes in peridotite xenoliths from the Premier diamond mine, South Africa: evidence for depletion and refertilisation of subcratonic lithosphere. International Kimberlite Conference: Extended Abstracts, 9. https://doi.org/10.29173/ikc3356

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Issue

Vol. 9 (2008): Vol 9: International Kimberlite Conference, Frankfurt

Section

Extended Abstracts

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