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单词 Armorican orogeny
释义

Armorican orogeny

英语百科

Variscan orogeny

(重定向自Armorican orogeny)
Location of the Hercynian-Alleghenian mountain belts in the middle of the Carboniferous period. Present day coastlines are indicated in grey for reference.[1]
Distribution of orogenies with similar ages to the Variscan orogeny (shaded)

The Variscan or Hercynian orogeny is a geologic mountain-building event caused by Late Paleozoic continental collision between Euramerica (Laurussia) and Gondwana to form the supercontinent of Pangaea.

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