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Orogenic belt
| Extended crust | Oceanic crust: 0–20 Ma 20–65 Ma >65 Ma |
An orogenic belt, orogen, or mobile belt,[a] is a zone of Earth's crust affected by orogeny.[2] An orogenic belt develops when a continental plate crumples and is uplifted to form one or more mountain ranges; this involves a series of geological processes collectively called orogenesis.[3][4]
- ^ "mobile belt". www.encyclopedia.com. Oxford University Press. Retrieved 2022-12-26.
- ^ "Orogenic belt | geology". Encyclopedia Britannica. Retrieved 2021-04-29.
- ^ Tony Waltham (2009). Foundations of Engineering Geology (3rd ed.). Taylor & Francis. p. 20. ISBN 978-0-415-46959-3.
- ^ Philip Kearey; Keith A. Klepeis; Frederick J. Vine (2009). "Chapter 10: Orogenic belts". Global Tectonics (3rd ed.). Wiley-Blackwell. p. 287. ISBN 978-1-4051-0777-8.
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