The Middle-upper Devonian clastic wedge of the Franklinian geosyncline

Bibliography: p. 259-274. Middle - Upper Devonian elastic strata in the Canadian Arctic Islands are present over an area of about 200,000 sq km (75,000 sq miles) and are up to 5000 m (16,000 1) thick. The strata comprise a elastic wedge which was deposited in the Franklinian geosyncline prior to Lat...

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Bibliographic Details
Main Author: Embry, Ashton F. (Ashton Fox)
Other Authors: Klovan, J. Edward
Format: Doctoral or Postdoctoral Thesis
Language:English
Published: University of Calgary 1976
Subjects:
Online Access:http://hdl.handle.net/1880/13662
https://doi.org/10.11575/PRISM/12466