| 書目名稱 | The Cordilleran Miogeosyncline in North America |
| 副標(biāo)題 | Geologic Evolution a |
| 編輯 | Henry V. Lyatsky,Vadim B. Lyatsky |
| 視頻video | http://file.papertrans.cn/907/906794/906794.mp4 |
| 概述 | Includes supplementary material: |
| 叢書名稱 | Lecture Notes in Earth Sciences |
| 圖書封面 |  |
| 描述 | 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. |
| 出版日期 | Book 1999 |
| 關(guān)鍵詞 | North America; Phanerozoic; Proterozoic; cordillera; evolution; geology; geophysics; history; megabelts; orog |
| 版次 | 1 |
| doi | https://doi.org/10.1007/BFb0017571 |
| isbn_softcover | 978-3-540-66197-9 |
| isbn_ebook | 978-3-540-48693-0Series ISSN 0930-0317 Series E-ISSN 1613-2580 |
| issn_series | 0930-0317 |
| copyright | Springer-Verlag Berlin Heidelberg 1999 |
|Archiver|手機版|小黑屋|
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