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The structure of the central part of the Soviet Arctic is a result of prolonged tectonic development which took place in seven main stages (tectonic periods). The structures formed comprised structural stages during each period respectively. The time limits of each stage were not entirely penecontemporaneous in adjacent regions. Thus, the main features of the tectonic development of the central Soviet Arctic are recurrent changes of the tectonic pattern and erosion processes at the end of each tectonic period and of each phase of its development. At the meeting of the First International Symposium on Arctic Geology held in Calgary, Alberta, Canada, January 11th to 13th, 1960, a number of instructive, interesting, and original papers on this topic were presented, and essentially all of them are printed in the pages of The Geology of the Arctic volumes I and II.
Geology --- Geognosy --- Geoscience --- Earth sciences --- Natural history --- Arctic Regions. --- Arctic --- Arctic Ocean Region --- Far North --- The Arctic --- Polar regions
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Geology, Stratigraphic --- Paleontology --- Geology --- Congresses --- Congresses --- Congresses.
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Geologie. --- Aardolie. --- Pétrole --- Géologie --- Petroleum --- Geology --- Geognosy --- Geoscience --- Earth sciences --- Natural history --- Coal-oil --- Crude oil --- Oil --- Caustobioliths --- Mineral oils --- Periodicals.
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As a result of the intensive search for oil and gas in western Canada, a regional meeting was held in 1955. This volume was the result of that meeting, and contains 23 papers divided between a discussion of the Jurassic and a discussion of the Carboniferous. Stratigraphy, subsurface, boundaries, formations, sedimentation and geology of western Canada and adjacent areas are thoroughly covered.
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Rocks, Sedimentary --- Sedimentation and deposition --- Congresses. --- Congresses.
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Geology, Stratigraphic --- Geology --- Stratigraphie --- Géologie
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