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|a 9783540486930
|9 978-3-540-48693-0
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|a 10.1007/BFb0017571
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|a Lyatsky, Henry V.
|e author.
|4 aut
|4 http://id.loc.gov/vocabulary/relators/aut
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|a The Cordilleran Miogeosyncline in North America
|h [electronic resource] :
|b Geologic Evolution and Tectonic Nature /
|c by Henry V. Lyatsky, Vadim B. Lyatsky.
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|a 1st ed. 1999.
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| 264 |
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|a Berlin, Heidelberg :
|b Springer Berlin Heidelberg :
|b Imprint: Springer,
|c 1999.
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|a XX, 388 p. 84 illus.
|b online resource.
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|a text
|b txt
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|a computer
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|a online resource
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|a text file
|b PDF
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|a Lecture Notes in Earth Sciences,
|x 0930-0317 ;
|v 86
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|a Governing principles in regional tectonic evolution -- Rock units in regional tectonic analysis -- Conceptual fundamentals of regional tectonic analysis on continents -- View of the cordilleran mobile megabelts evolution from the craton -- Omineca orogenic belt as tectonotype of the Eastern Cordilleran miogeosyncline -- Broad look at geodynamial mechanisms of crustal restructuring in the Cordilleran orogens and median massifs -- Lessons from Cordilleran geology for the methodology of regional tectonic analysis of mobile megabelts -- Practical utility of rock evidence and geophysical studies in restoring regional tectonic history in mobile megabelts.
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|a Steep crustal-scale faults, having their origins in the Late Archean and Early Proterozoic and trending NE-SW, which define the fundamental block lithospheric structure of the North American craton, are seen from geological and geophysical evidence to continue far into the interior of the Late Proterozoic-Phanerozoic Canadian Cordilleran mobile megabelt. This suggests that variously reworked ex-cratonic basement blocks underlie much of the Cordillera. The western edge of the modern craton is probably near the Rocky Mountain-Omineca belt boundary, where Cordilleran tectonic reworking of the crystalline crust is first encountered; the Rocky Mountain fold-and-thrust belt on the east side of the Cordillera is evidently rootless and overlies the undisturbed cratonic basement. Phanerozoic differences between the Cordilleran tectonic belts, resulting from a long, dissimilar, multi-cycle history of waxing and waning orogenesis apparent from the rock record, lie chiefly in the degree of indigenous tectonic remobilization and reworking of the ancient crust.
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|a Geology.
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|a Sedimentology.
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|a Geophysics.
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|a Geology.
|0 http://scigraph.springernature.com/things/product-market-codes/G17002
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|a Sedimentology.
|0 http://scigraph.springernature.com/things/product-market-codes/G17080
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|a Geophysics/Geodesy.
|0 http://scigraph.springernature.com/things/product-market-codes/G18009
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| 700 |
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|a Lyatsky, Vadim B.
|e author.
|4 aut
|4 http://id.loc.gov/vocabulary/relators/aut
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| 710 |
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|a SpringerLink (Online service)
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| 773 |
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|t Springer eBooks
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|i Printed edition:
|z 9783540661979
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| 776 |
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|i Printed edition:
|z 9783662166987
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| 830 |
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|a Lecture Notes in Earth Sciences,
|x 0930-0317 ;
|v 86
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| 856 |
4 |
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|u https://doi.org/10.1007/BFb0017571
|z Full Text via HEAL-Link
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|a ZDB-2-EES
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|a ZDB-2-BAE
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| 950 |
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|a Earth and Environmental Science (Springer-11646)
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