تجبل لاراميد
تجبل لاراميد Laramide orogeny، هو أحدث مراحل الثورة الألبية، نشطت خلال نهاية العصر الطباشيري والثالث المبكر، مسجلة بوضوح سلسلة جبال روكي في غرب أمريكا الشمالية.[1]
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عواقب بيئية
الأحواض والجبال
انظر أيضا
- The earlier Sevier orogeny
- The still-earlier Nevadan orogeny of the late Jurassic — early Cretaceous.
- Geology of the Rocky Mountains
- Geology of the Pacific Northwest
الهوامش
المصادر
- English, Joseph M.; Johnston, Stephen T. (2004). "The Laramide Orogeny: What Were the Driving Forces?". International Geology Review. 46: 833–838. doi:10.2747/0020-6814.46.9.833.
- Lehman, T. M. (2001). "Late Cretaceous dinosaur provinciality". In Tanke, D. H.; Carpenter, K. (eds.). Mesozoic Vertebrate Life. Indiana University Press. pp. 310–328.
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(help) - Liu, L.; Gurnis, M.; Seton, M.; Saleeby, J.; Müller, R.D.; Jackson, J.M. (2010). "The role of oceanic plateau subduction in the Laramide orogeny" (PDF). Nature Geoscience. 3 (5): 353–357. doi:10.1038/ngeo829.
- Richard F. Livaccari, Kevin Burke, and AMC Sengor (1981). "Was the Laramide orogeny related to subduction of an oceanic plateau?". Nature. 289 (5795): 276–278. doi:10.1038/289276a0.
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: CS1 maint: multiple names: authors list (link) - Saleeby, Jason (2003). "Segmentation of the Laramide Slab -- Evidence from the southern Sierra Nevada region". Geological Society of America Bulletin. 115: 655–668.
- W. P. Schellart, D. R. Stegman, R. J. Farrington, J. Freeman, and L. Moresi (16 July 2010). "Cenozoic Tectonics of Western North America Controlled by Evolving Width of Farallon Slab". Science. 329 (5989): 316–319. doi:10.1126/science.1190366. PMID 20647465.
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: CS1 maint: multiple names: authors list (link) - Willis, Grant C. (2000). "I thought that was the Laramide orogeny!". Utah's Sevier Thrust System. Utah Geological Survey.
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(help)
وصلات خارجية
الكلمات الدالة: