Devonian stratigraphy of the southern Canadian Rocky Mountains
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Devonian stratigraphy of the southern Canadian Rocky Mountains

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Published by International Geological Congress in Montreal .
Written in English

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Open LibraryOL22013537M

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Stratigraphy of the Canadian Rocky Mountains in the Banff area. Let’s take a look at the general geological setting of Canada. In a nutshell, where the central craton of the continent is exposed in northern Saskatchewan, Manitoba, Ontario, Quebec, Nunavut and the Northwest Territories, it is called the Canadian Shield. The Devonian (/ d ɪ ˈ v oʊ n. i. ən, d ə-, d ɛ-/ dih-VOH-nee-ən, də-, deh-) is a geologic period and system of the Paleozoic, spanning 60 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, where rocks from this period were first studied.. The first significant adaptive radiation. Devonian Period - Devonian Period - Devonian geology: The union of the paleocontinents of Laurentia and Baltica occurred near the beginning of the Devonian to form a single landmass that has been referred to both as Laurussia and as Euramerica. The northern portion of the combined landmass gave rise to widespread areas of continental desert, playa, and alluvial plain deposits that form one of. Future Devonian Meetings: 5th IPC - International Palaeontological Congress. Paris (France) July The Subcommission on. Devonian Stratigraphy. Latest News. SDS Newsletter 32 ().

Book Chapter Cratonic-Margin and Antler-Age Foreland Basin Strata (Middle Devonian to Lower Carboniferous) of the Southern Canadian Rocky Mountains and Adjacent Plains Author(s) Lauret E. Savoy Lauret E. Savoy 1. Department of Geography and Geology, Mount Holyoke College, South Hadley, MA   The southern termination of the Western Main Ranges of the Canadian Rockies, near Fort Steele, British Columbia: Stratigraphy, structure, and tectonic implications. Geology of the Rocky Mountains West of Calgary, Alberta, in the Kananaskis West Half Map Area (82J)* (Figure 1). Major changes in stratigraphy and structural style occur across the area. The southern Canadian Rocky Mountains Fold and Thrust belt. The Southern Canadian Rocky Mountains extends westward from the essentially flat-lying strata of the Interior Plains to the Southern Rocky Mountain trench, a long, narrow valley con-.

Keywords: Rocky Mountains, Canada, faults, orogeny, geochronology, gouge. Figure 1. Location map of gouge samples in Canadian Rockies analyzed in this study. Details of sites are presented in Table 1. INTRODUCTION The Rocky Mountains of southern Canada are a classic area for the study of fold-and-thrust belt development. Spatial and temporalFile Size: KB. Unformatted text preview: STRATIGRAPHY AND CORRELATION OF THE JURASSIC IN THE CANADIAN ROCKY MOUNTAINS AND ALBERTA FOOTHILLS1 HANS FREBOLD2 Ottawa, Ontario ABSTRACT The Jurassic of the Canadian Rocky Mountains and foothills comprising the Fernie group and the lower part of the Kootenay and Nikanassin formations is subdivided on a paleontological basis . Book" reporting the results of Captain Palliser's expedition to the Cana-dian west in which James Hector () published the first geologic observations on the Canadian Rocky Mountains. Today the Southern Canadian Rockies rank among the best known mountain ranges of . Geologic history, stratigraphy & tectonics. The Precambrian granite and gneiss crystalline basement rocks beneath Alberta are extremely ancient, dating to the Archean and Slave Craton and Southern Alberta craton are the oldest units at more billion years old, while younger units from the Proterozoic include the Wopmay orogeny, Great Slave Lake shear zone, Pre-Taltston.