Late/Post Variscan Orocline Formation and Widespread Magmatism
Abstract
The Paleozoic geology of Iberia is dominated by the tectonics of the Variscan orogeny and its aftermath. This defining geologic event was the result of large-scale collision that involved amalgamation of multiple continents and micro-continents, the closure of oceanic basins and eventual orogenic collapse, and finally modification and oroclinal bending during the waning stages of Pangea amalgamation. Existing data from the western Variscan...
Paper Details
Title
Late/Post Variscan Orocline Formation and Widespread Magmatism
Published Date
Jan 1, 2019
Journal
Pages
527 - 542
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