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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Λεπτομέρειες βιβλιογραφικής εγγραφής
Κύριοι συγγραφείς: Lyatsky, Henry V. (Συγγραφέας, http://id.loc.gov/vocabulary/relators/aut), Lyatsky, Vadim B. (http://id.loc.gov/vocabulary/relators/aut)
Συγγραφή απο Οργανισμό/Αρχή: SpringerLink (Online service)
Μορφή: Ηλεκτρονική πηγή Ηλ. βιβλίο
Γλώσσα:English
Έκδοση: Berlin, Heidelberg : Springer Berlin Heidelberg : Imprint: Springer, 1999.
Έκδοση:1st ed. 1999.
Σειρά:Lecture Notes in Earth Sciences, 86
Θέματα:
Διαθέσιμο Online:Full Text via HEAL-Link
Πίνακας περιεχομένων:
  • 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.