Map of features associated with the Ungava magmatic event

The Ungava magmatic event was a widespread magmatic event that began about 2.22 billion years ago during the Proterozoic Eon.

Extent

With an area of 170,000 km2 (66,000 sq mi), the Ungava magmatic event caused the formation of a large igneous province.[1] Magmatic features that were formed during the Ungava magmatic event include the Klotz, Maguire and Senneterre dikes of Quebec and the Nipissing sills of Ontario.[2]

References

  1. ↑ 2000 Ma large mafic magmatic events
  2. ↑ "Regional Metallogeny Large Igneous Provinces in Canada Through Time and Their Metallogenic Potential". Mineral Deposits of Canada. Geological Survey of Canada. 2008-09-25. Archived from the original on 2010-04-20. Retrieved 2010-05-17.

57°22′52″N 68°49′34″W / 57.381°N 68.826°W / 57.381; -68.826

This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.