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

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

doi:10.29173/ikc3378

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