Jump to content

K6 pipe

Add links
From Wikipedia, the free encyclopedia

This is the current revision of this page, as edited by Volcanoguy (talk | contribs) at 04:54, 16 August 2023 (ce). The present address (URL) is a permanent link to this version.

(diff) ← Previous revision | Latest revision (diff) | Newer revision → (diff)

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 this part of Alberta was volcanically active during the Late Cretaceous period.[1] It is typical of melts that originated from the lower mantle.[2]

See also

[edit]

References

[edit]
  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


Stub icon

This Northern Alberta location article is a stub. You can help Wikipedia by expanding it.

Retrieved from "https://en.wikipedia.org/w/index.php?title=K6_pipe&oldid=1170619847"