Geodynamic evolution of a Cadomian arc region: the northern Ossa-Morena zone, Iberian massif-Reference-Cited by-同舟云学术

Geodynamic evolution of a Cadomian arc region: the northern Ossa-Morena zone, Iberian massif

Published:2002-07 Issue:1-2 Volume:352 Page:105-120
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Bandres A.,Eguı́luz L.,Gil Ibarguchi J.I.,Palacios T.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference87 articles.

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2. Variscan shear-zone deformation of late PreCambrian basement in SW Iberia, implications for circum-Atlantic pre-Mesozoic tectonics;Ábalos;J. Struct. Geol.,1992

3. Correlation between seismic anisotropy and major geological structures in SW Iberia: a case study on continental lithosphere deformation;Ábalos;Tectonics,1995

4. Constitución tectono-estratigráfica del Corredor Blastomilonı́tico de Badajoz–Córdoba: nueva propuesta de subdivisión;Ábalos;Geogaceta,1990

5. Cadomian subduction/collision and variscan transpression the Badajoz–Córdoba Shear Belt (SW Spain);Ábalos;Tectonophysics,1991

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