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How Stiff Was Armorica During the Variscan Orogeny? A Reappraisal of the “B…
In collision belts, the upper plate is generally less deformed than the lower one that underwent syn-metamorphic ductile shearing, and frequently late-collisional crustal melting. Concerning the Variscan orogeny, it is widely accepted that the Armorica microcontinent represented the upper plate of the collision system. In France, the Central-North-Armorican Domain belonged to this upper plate w…
- Edisi
- Vol.15, Issue 2, February 2025
- ISBN/ISSN
- 2076-3263
- Deskripsi Fisik
- 30 hlm PDF, 12.067 KB
- Judul Seri
- Geosciences
- No. Panggil
- 550
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