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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Format: | Doctoral or Postdoctoral Thesis |
Language: | English |
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University of Calgary
1976
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Online Access: | http://hdl.handle.net/1880/13662 https://doi.org/10.11575/PRISM/12466 |