hercynian orogeny wikipedia - EAS
- The Variscan orogeny (Hercynian orogeny) is an ancient mountain-building event in the late Palaeozoic era. It was caused by a continental collision between Euramerica (Laurussia) and Gondwanato form the supercontinent of Pangaea.
Gondwana
Gondwana, was a supercontinent that existed from the Neoproterozoic until the Jurassic. It was formed by the accretion of several cratons. Eventually, Gondwana became the largest piece of continental crust of the Paleozoic Era, covering an area of about 100,000,000 km². During the Carb…
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The Variscan orogeny involved a complicated heterogeneous assembly of different microplates and heterochronous collisions, making the exact reconstruction of the plate tectonic processes difficult. Plate convergence that caused the Caledonian orogeny in the Silurian continued to form … See more
The Variscan or Hercynian orogeny was a geologic mountain-building event caused by Late Paleozoic continental collision between Euramerica (Laurussia) and Gondwana to form the supercontinent of Pangaea See more
• Christopher R. Scotese, Paleomap Project:
• Ronald Blakey, Colorado Plateau Geosystems Inc: Europe in the Late Carboniferous Archived 2015-09-22 at the Wayback Machine See moreThe name Variscan, comes from the Medieval Latin name for the district Variscia, the home of a Germanic tribe, the Varisci; Eduard Suess, professor of geology at the University of Vienna, coined the term in 1880. (Variscite, a rare green mineral first discovered in the See more
• Matte, P. (2001). "The Variscan collage and orogeny (480 ±290 Ma) and the tectonic definition of the Armorica microplate: a … See more
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WebCategory:Hercynian orogeny - Wikipedia Help Category:Hercynian orogeny Geology portal Wikimedia Commons has media related to Variscan orogeny. This category …
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WebHercynian Orogeny. The Variscan orogeny is the consequence of the closure of the Rheic ocean, and subsequent collision of Laurussia that was driven by a southward oceanic …
- https://en.wikipedia.org/wiki/List_of_orogenies
• Saamian orogeny – Formation of an extensive area of tonalitic-trondhjemitic crust in Fennoscandia, (3.1–2.9 Ga)
• Lopian orogeny – Archean orogeny – Formation of two different types of terrain compatible with plate tectonic concepts. One is a belt of high-grade gneisses formed in a regime of strong mobility, while the other is a region of granitoid intrusions and greenstone belts surrounded by the remnants of a Saamian substratum, (2.9–2.6 Ga)Wikipedia · Text under CC-BY-SA license- Estimated Reading Time: 6 mins
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WebHercynian orogeny A major and prolonged episode of mountain building that began in the Late Devonian and continued throughout the Carboniferous, affecting a broad belt along …
- https://en.wikipedia.org/wiki/Alleghanian_orogeny
WebThe Alleghanian orogeny or Appalachian orogeny is one of the geological mountain-forming events that formed the Appalachian Mountains and Allegheny Mountains. The …
- https://en.wikipedia.org/wiki/Hercynia
WebHyrcania (disambiguation) Hercynian orogeny, a synonym for the Variscan orogeny of the Carboniferous Hercynian massifs, part of the Massif Central of France This …
- https://en.wikipedia.org/wiki/Caledonian_orogeny
WebThe Caledonian orogeny was a mountain-building era recorded in the northern parts of the British Isles, the Scandinavian Mountains, Svalbard, eastern Greenland and parts of …
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