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Franklin dike swarm

From Wikipedia, the free encyclopedia
Large geological structure in Canada
Franklin dike ofolivinegabbro intrusive, on northwestern Baffin Island, betweenPond Inlet andArctic Bay.

TheFranklin dike swarm, also called theFranklin dikes, is aProterozoicdike swarm of theFranklin Large Igneous Province inNorthern Canada. It is one of the several major magmatic events in theCanadian Shield and it was formed 723 million years ago. Areas in the Franklin have been prospected fornickel,copper, andplatinum group metals.[1]

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 mi2).[2]

See also

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References

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  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 fromthe original on 2010-04-20. Retrieved2009-07-19.
  2. ^Reconstructing Ancient Continents Using the Large Igneous Province Record: Implications For Mineral, Hydrocarbon, and Earth Systems
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