The Cordilleran Miogeosyncline in North America

Geologic Evolution and Tectonic Nature

Nonfiction, Science & Nature, Science, Earth Sciences, Geology
Cover of the book The Cordilleran Miogeosyncline in North America by Henry V. Lyatsky, Vadim B. Lyatsky, Springer Berlin Heidelberg
View on Amazon View on AbeBooks View on Kobo View on B.Depository View on eBay View on Walmart
Author: Henry V. Lyatsky, Vadim B. Lyatsky ISBN: 9783540486930
Publisher: Springer Berlin Heidelberg Publication: April 10, 2006
Imprint: Springer Language: English
Author: Henry V. Lyatsky, Vadim B. Lyatsky
ISBN: 9783540486930
Publisher: Springer Berlin Heidelberg
Publication: April 10, 2006
Imprint: Springer
Language: English
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; 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.
View on Amazon View on AbeBooks View on Kobo View on B.Depository View on eBay View on Walmart
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; 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.

More books from Springer Berlin Heidelberg

Cover of the book Histopathology of the Endometrium by Henry V. Lyatsky, Vadim B. Lyatsky
Cover of the book Biofilm Highlights by Henry V. Lyatsky, Vadim B. Lyatsky
Cover of the book Risk Management and Governance by Henry V. Lyatsky, Vadim B. Lyatsky
Cover of the book A Concise Guide to Market Research by Henry V. Lyatsky, Vadim B. Lyatsky
Cover of the book Synchrotron Radiation by Henry V. Lyatsky, Vadim B. Lyatsky
Cover of the book Fairness als Führungskompetenz by Henry V. Lyatsky, Vadim B. Lyatsky
Cover of the book Scientific Basis of Cancer Chemotherapy by Henry V. Lyatsky, Vadim B. Lyatsky
Cover of the book Decision Tools for Radiation Oncology by Henry V. Lyatsky, Vadim B. Lyatsky
Cover of the book Web-basierte Anwendungen Virtueller Techniken by Henry V. Lyatsky, Vadim B. Lyatsky
Cover of the book Tropospheric Ozone Abatement by Henry V. Lyatsky, Vadim B. Lyatsky
Cover of the book Cardiovascular Surgery 1980 by Henry V. Lyatsky, Vadim B. Lyatsky
Cover of the book Environmental Photochemistry by Henry V. Lyatsky, Vadim B. Lyatsky
Cover of the book Total Addiction by Henry V. Lyatsky, Vadim B. Lyatsky
Cover of the book Ionic Liquids by Henry V. Lyatsky, Vadim B. Lyatsky
Cover of the book Diseases of the Salivary Glands Including Dry Mouth and Sjögren’s Syndrome by Henry V. Lyatsky, Vadim B. Lyatsky
We use our own "cookies" and third party cookies to improve services and to see statistical information. By using this website, you agree to our Privacy Policy