Franklin dike swarm

The Franklin dike swarm, also called the Franklin dikes, is a Proterozoic dike swarm of the Franklin Large Igneous Province in Northern Canada. It is one of the several major magmatic events in the Canadian Shield and it was formed 723 million years ago. Areas in the Franklin have been prospected for nickel, copper, and platinum group metals.[1]

Franklin dike of olivine gabbro intrusive, on northwestern Baffin Island, between Pond Inlet and Arctic Bay.

The Franklin dike swarm occupies a major part of the Franklin Large Igneous Province, which covers an area of more than 2,000,000 km2 (770,000 sq mi).[2]

See also

References
  1. "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 2009-07-19.
  2. Reconstructing Ancient Continents Using the Large Igneous Province Record: Implications For Mineral, Hydrocarbon, and Earth Systems
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.