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...
Kaydedildi:
| Asıl Yazarlar: | , |
|---|---|
| Materyal Türü: | Livre numérique |
| Dil: | Anglais |
| Baskı/Yayın Bilgisi: |
Berlin [etc.] :
Springer
[20..].
Cham : Springer Nature |
| Seri Bilgileri: | Lecture notes in Earth sciences
86 |
| Konular: | |
| Online Erişim: | Accès sur la plateforme de l'éditeur Accès sur la plateforme Istex Accès Université d'Orléans Accès INSA CVL |
| Not: |
Archives Springer e-books (Licence nationale) Archives Springer e-books (Licence nationale) |
| Autres localisations: | Voir dans le Sudoc |
| 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 |