Lac de Gras kimberlite field

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Diavik Diamond Mine consists of three diatremes associated with the Lac de Gras kimberlite field Diavik Diamond Mine.jpg
Diavik Diamond Mine consists of three diatremes associated with the Lac de Gras kimberlite field
Fort a la Corne-Lac de Gras kimberlites Fort a la Corne-Lac de Gras kimberlites.png
Fort à la Corne-Lac de Gras kimberlites

The Lac de Gras kimberlite field is a group of Late Cretaceous to Eocene age diatremes in the Northwest Territories, Canada. [1]

The Eocene (ca. 55-50 Ma) age diatremes of the Lac de Gras kimberlite field support two world-class diamond mines called Ekati and Diavik. [2] Ekati, Canada's first diamond mine, [3] has produced 40,000,000 carats (8,000 kg) of diamonds out of six open pits between 1998 and 2008, [3] while Diavik to the southeast has produced 35,400,000 carats (7,080 kg) of diamonds since its foundation in 2003. [4]

See also

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The Attawapiskat kimberlite field is a field of kimberlite pipes located astride the Attawapiskat River in the Hudson Bay Lowlands, in Northern Ontario, Canada. It is thought to have formed about 180 million years ago in the Jurassic period when the North American Plate moved westward over a centre of upwelling magma called the New England hotspot, also referred to as the Great Meteor hotspot.

The Buffalo Head Hills kimberlite field is a group of kimberlitic volcanic pipes or diatremes in north-central Alberta, Canada. As of 2011, 41 kimberlite pipes, of which 28 are diamondiferous, had been identified in the field. They were emplaced during Late Cretaceous to early Paleocene time.

The Birch Mountains kimberlite field is a cluster of kimberlitic volcanic pipes or diatremes in north-central Alberta, Canada that were emplaced during a period of kimberlitic volcanism in the Late Cretaceous epoch. As of 2011, 8 diatremes had been discovered in the field, and diamonds and microdiamononds had been recovered during sampling programs.

The Misery Kimberlite Complex is a diatreme cluster in the Northwest Territories of Northern Canada. It was formed approximately 56 million years ago by several overlapping explosive eruptions and intrusions. All seem to have been structurally controlled by zones of weakness related with faults, dikes and a major contact in the Archean basement. The complex is associated with a field of diamondiferous kimberlites called the Lac de Gras kimberlite field.

K19 pipe is a diatreme in the southwestern part of the Buffalo Head Hills kimberlite field in Northern Alberta, Canada. It is thought to have formed about 60 million years ago, making it one of the youngest volcanic formations in the Buffalo Head Hills kimberlite field and in Alberta. Unlike many other diatremes in the Buffalo Head Hills kimberlite field, it contains low diamond content.

<span class="mw-page-title-main">Hugo Dummett</span>

Hugo T. Dummett (1940–2002) was a South African mineral-exploration geologist who is best known for his role in the discovery of the Ekati Diamond Mine in the Barren Lands of Canada's Northwest Territories. Dummett has been described as "the brains, the ideas and the energy" behind the discovery of Ekati, which led to the creation of a new Canadian diamond-mining industry.

References

  1. Intensive Variables in Kimberlite Magmas, Lac de Gras, Canada and Implications for Diamond Survival
  2. North Arrows Minerals Inc.: Lac de Gras Project Archived 2010-06-09 at the Wayback Machine
  3. 1 2 Zlotnikoc, Dan (November 2008). "A northern star - Canada's first diamond mine celebrates a milestone". CIM Magazine. Montreal, Quebec, Canada. 3 (7): 40–43. ISSN   1718-4177.
  4. "Diavik diamond mine in N.W.T gets new development money". CBC News. 2007-11-26. Retrieved 2009-01-25.