Origin of diamondiferous Torngat ultramafic lamprophyres and the role of multiple MARID-type and carbonatitic vein metasomatized cratonic mantle in the genesis of SiO2-poor potassic melts

Authors

  • S. Tappe
  • S.F. Foley
  • B.A. Kjarsgaard
  • R.L. Romer
  • L.M. Heaman
  • A. Stracke
  • G.A. Jenner

DOI:

https://doi.org/10.29173/ikc3378

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Published

2008-10-15

How to Cite

Tappe, S., Foley, S., Kjarsgaard, B., Romer, R., Heaman, L., Stracke, A., & Jenner, G. (2008). Origin of diamondiferous Torngat ultramafic lamprophyres and the role of multiple MARID-type and carbonatitic vein metasomatized cratonic mantle in the genesis of SiO2-poor potassic melts. International Kimberlite Conference: Extended Abstracts, 9. https://doi.org/10.29173/ikc3378

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