Deformation associated with gypsum karst in the Salt River Escarpment, northeastern Alberta

An escarpment formed by the carbonate Keg River and evaporitic Chinchaga formations of Middle Devonian age extends southwards from the Slave River 30 km west of Fort Smith, Northwest Territories. Newly described folds in the bedrock are due to hydration of the anhydrite to gypsum in the Chinchaga Fo...

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Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Authors: Tsui, Po C., Cruden, David M.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1984
Subjects:
Online Access:http://dx.doi.org/10.1139/e84-099
http://www.nrcresearchpress.com/doi/pdf/10.1139/e84-099