Bear River dikes

The Bear River dikes are a 1,265 to 1,269 million year old group of dikes in northern Yukon, Canada. They represent a feature related to magmatism of the extensive Mackenzie Large Igneous Province and are considered to be the western extension of the northwest–southeast trending Mackenzie dike swarm.^[1]

References[edit]

^ Schwab, Danette L.; Thorkelson, Derek J.; Mortensen, James K.; Creaser, Robert A.; Abbott, J. Grant (2004-08-20). "The Bear River dykes (1265-1269 Ma): westward continuation of the Mackenzie dyke swarm into Yukon, Canada". Precambrian Research. 133 (3–4): 175. Bibcode:2004PreR..133..175S. CiteSeerX 10.1.1.607.3240. doi:10.1016/j.precamres.2004.04.004.

This article about a Yukon location is a stub. You can help Wikipedia by expanding it.

This article about a specific Canadian geological feature is a stub. You can help Wikipedia by expanding it.

[1] Schwab, Danette L.; Thorkelson, Derek J.; Mortensen, James K.; Creaser, Robert A.; Abbott, J. Grant (2004-08-20). "The Bear River dykes (1265-1269 Ma): westward continuation of the Mackenzie dyke swarm into Yukon, Canada". Precambrian Research. 133 (3–4): 175. Bibcode:2004PreR..133..175S. CiteSeerX 10.1.1.607.3240. doi:10.1016/j.precamres.2004.04.004.

[1]