2-D thermal modeling of HT–LP metamorphism in NW and Central Iberia: Implications for Variscan magmatism, rheology of the lithosphere and orogenic evolution-Reference-Cited by-同舟云学术

2-D thermal modeling of HT–LP metamorphism in NW and Central Iberia: Implications for Variscan magmatism, rheology of the lithosphere and orogenic evolution

Published:2015-08 Issue: Volume:657 Page:21-37
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Alcock James E.,Martínez Catalán José R.,Rubio Pascual Francisco J.,Montes Alejandro Díez,Fernández Rubén Díez,Barreiro Juan Gómez,Arenas Ricardo,Dias da Silva Ícaro^ORCID,Clavijo Emilio González

Funder

Spanish Ministry of Science and Innovation

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

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3. Use of thermal modeling to assess the tectono-metamorphic history of the Lugo and Sanabria gneiss domes, Northwest Iberia;Alcock;Bull. Soc. Geol. Fr.,2009

4. One and two-dimensional models are equally effective in monitoring the crust's thermal response to advection by large-scale thrusting during orogenesis;Alcock;Comput. Geosci.,2011

5. Large-scaleflat-lying isoclinal folding in extending lithosphere: Santa María de la Alameda dome (Central Iberian Massif, Spain);Arango;Lithosphere,2013

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