A revision of the stratigraphy of the Lea Park formation in west central Saskatchewan
The Lea Park formation is an equivalent of the Upper Cretaceous Milk River and Pakowki formations of southern Alberta. Upper Cretaceous sediments of the Prairie Provinces are derived from land masses which bordered the Western geosyncline. Redistribution of Upper Cretaceous non-marine sediments from...
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| Language: | English |
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University of British Columbia
2012
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| Online Access: | http://hdl.handle.net/2429/41898 |