The cordilleran miogeosyncline in North America : geologic evolution and tectonic nature

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 Prote...

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Opis bibliograficzny
Główni autorzy: Lyatsky, Henry, 1962-, Lyatsky, Vadim B., 1927- (Autor)
Format: Livre numérique
Język:Anglais
Wydane: Berlin [etc.] : Springer [20..].
Cham : Springer Nature
Seria:Lecture notes in Earth sciences 86
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Komentarz: Archives Springer e-books (Licence nationale)
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Edition sous un autre format:• The cordilleran miogeosyncline in North America, geologic evolution and tectonic nature, Henry V. Lyatsky and Vadim B. Lyatsky, New York, Springer, 1999, 1 vol. (384 p.), Lecture notes in earth sciences, 978-3-540-66197-9
• The Cordilleran Miogeosyncline in North America, Texte imprimé, 9783662166987
Spis treści:
  • 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.