Variscan orogeny
(重定向自Variscan)
![Location of the Hercynian-Alleghenian mountain belts in the middle of the Carboniferous period. Present day coastlines are indicated in grey for reference.[1]](/Images/godic/202502/19/Hercynides_EN.svg5516.png")

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.
单词 | Variscan |
释义 |
Variscan
英汉-汉英词典
华力西期
词组 | 习惯用语
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Variscan orogeny 华力斯坎造山运动 网络短语:Variscan mountains 华力西山地 Variscan stage 华力西阶段 middle Variscan stage 华力西中期 Variscan 华力西; 造山运动; Late Variscan 华力西晚期侵入岩 mid-late Variscan 海西中晚期 Variscan Unconformable Contact 华力西不整合面控矿 Late Caledonian Early Variscan 加里东晚期 Middle Variscan-Indosinian stage 构造岩浆阶段
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Variscan orogeny(重定向自Variscan)
![]() ![]() 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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