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...
| Κύριοι συγγραφείς: | , |
|---|---|
| Συγγραφή απο Οργανισμό/Αρχή: | |
| 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.