K6 pipe

From Infogalactic: the planetary knowledge core
Jump to: navigation, search

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


<templatestyles src="Asbox/styles.css"></templatestyles>

Stub icon

This Northern Alberta location article is a stub. You can help Wikipedia by expanding it.
Retrieved from "https://infogalactic.com/w/index.php?title=K6_pipe&oldid=400095731"