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K6 pipe

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This is an old revision of this page, as edited by Volcanoguy (talk | contribs) at 09:36, 2 December 2010 (→See also: Volcanism of Canada portal). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

K6 pipe is a diamondiferous diatreme in the Buffalo Head Hills kimberlite field of Northern Alberta, Canada. It is thought to have formed about 85 million years ago when is part of Alberta was volcanically active during the Late Cretaceous period.[1] It is typical of melts that originated from the low mantle.[2]

See also

References

  1. ^ Emplacement characteristics of Late Cretaceous and Paleocene pyroclastic and injected kimberlites in northern Alberta, Canada
  2. ^ Alberta Geological Survey: Radiogenic Isotope Geochemistry of Kimberlitic Rocks in Northern Alberta: Constraints for Source of Magmatism and Emplacement Age


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