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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Detalhes bibliográficos
Autor principal: Ribeiro, M.L. (author)
Outros Autores: 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)
Formato: bookPart
Idioma:eng
Publicado em: 2020
Assuntos:
Variscan cycle
LP-HT complexes
Cambrian-Early Ordovician rift stage
HP-LT complexes
Subduction
MP and LP/HT complexes
Syn-to-post-collision
Texto completo:http://hdl.handle.net/10773/28854
País:Portugal
Oai:oai:ria.ua.pt:10773/28854

Texto Completo

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

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