Variscan Metamorphism

Various segments of Variscan crust are currently exposed in Iberia in response to successive tectonic events during the Variscan orogeny itself and subsequent extensional and compressive events during the Alpine cycle, all accompanied by surface erosion, and collectively contributing to their exhuma...

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Bibliographic Details
Main Author: Ribeiro, M.L. (author)
Other Authors: Reche, J. (author), López-Carmona, A. (author), Aguilar, C. (author), Bento dos Santos, T. (author), Chichorro, M. (author), Dias da Silva, Í. (author), Díez-Montes, A. (author), González-Clavijo, E. (author), Gutiérrez-Alonso, G. (author), Leal, N. (author), Liesa, M. (author), Martínez, F.J. (author), Mateus, A. (author), Mendes, Maria Helena Acciaioli (author), Moita, P. (author), Pedro, J. (author), Quesada, C. (author), Santos, José Francisco (author), Solá, A.R. (author), Valverde-Vaquero, P. (author)
Format: bookPart
Language:eng
Published: 2020
Subjects:
Variscan cycle
LP-HT complexes
Cambrian-Early Ordovician rift stage
HP-LT complexes
Subduction
MP and LP/HT complexes
Syn-to-post-collision
Online Access:http://hdl.handle.net/10773/28854
Country:Portugal
Oai:oai:ria.ua.pt:10773/28854

Internet

http://hdl.handle.net/10773/28854

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