Journal Article10.1038/288329A0
Cordilleran suspect terranes
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TL;DR: The North American Cordillera is made up of "suspect terranes" as discussed by the authors, which are allochthonous to the North American continent and seem to have been swept from far reaches of the Pacific Ocean before collision and accretion into the Cordilleran margin mostly in Mesozoic to early Cenozoic time.
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Abstract: Over 70% of the North American Cordillera is made up of ‘suspect terranes’. Many of these geological provinces are certainly allochthonous to the North American continent and seem to have been swept from far reaches of the Pacific Ocean before collision and accretion into the Cordilleran margin mostly in Mesozoic to early Cenozoic time.
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Citations
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References
Cenozoic Tectonics of Asia: Effects of a Continental Collision: Features of recent continental tectonics in Asia can be interpreted as results of the India-Eurasia collision.
Peter Molnar,Paul Tapponnier +1 more
TL;DR: The JSTOR Archive is a trusted digital repository providing for long-term preservation and access to leading academic journals and scholarly literature from around the world, supported by libraries, scholarly societies, publishers, and foundations.
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Implications of Plate Tectonics for the Cenozoic Tectonic Evolution of Western North America
TL;DR: In this paper, the authors examined the history of plate motions between the American and Pacific plates in the late Cenozoic and found that the two plates were fixed with respect to one another until 5 m.y.
1.9K
Cordilleran Benioff zones
TL;DR: In this article, a magmatic arc initiated near the continental margin, swept over 1,000 km northeastward, then swept back, all in 110 Myr, was interpreted as due to flattening of a Benioff zone to < 15° followed by rapid collapse.
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•Book
Mesozoic paleogeography of the Western United States
D. G. Howell,Kristin A. McDougall,Mineralogists. Pacific Section +2 more
- 01 Jan 1978
399
Paleopoles and paleolatitudes of North America and speculations about displaced terrains
TL;DR: A statistically determined path of apparent polar wander for the past 300 million years for North America is given in this paper, which has a zigzag form, the bends corresponding to important changes in the drift of North America.
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