Geology of Manitoba explained

In central Manitoba lies the Flin Flon greenstone belt, which is one of the largest Paleoproterozoic volcanic-hosted massive sulphide districts in the world, containing 27 copper-zinc-(gold) deposits from which more than 183 million tonnes of sulphide have been mined.[1]

Ashville Formation

See main article: Ashville Formation. The Ashville Formation is a geological formation in Saskatchewan and Manitoba whose strata date back to the Late Cretaceous. Dinosaur remains are among the fossils that have been recovered from the formation.[2]

It is geochronologically equivalent to the Lower Colorado Group and the Viking Formation in central Alberta.

Notes and References

  1. Norris, Jessica . Report on the 2007 Diamond Drilling Program McClarty Lake Project, Manitoba . Aurora Geosciences Ltd. . 2007 . 2008-02-22 . dead . https://web.archive.org/web/20080530010956/http://www.troymet.com/i/pdf/2007McClarty43-101.pdf . 2008-05-30 .
  2. Weishampel, David B; et al. (2004). "Dinosaur distribution (Late Cretaceous, North America)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 574-588. .