3D geological modelling of a polyphase deformed pre-Variscan IOCG mineralization located at the southeastern border of the Ossa Morena Zone, Iberian Massif (Spain)

Author:

Gumiel Pablo,Arias Mónica,Martín-Izard Agustín

Publisher

Wiley

Subject

Geology

Reference36 articles.

1. Abalos , B. 1990 Cinemática y mecanismos de la deformación en régimen de transpresión: Evolución estructural y metamórfica de la Zona de cizalla dúctil de Badajoz-Córdoba

2. The use of conic sections for the geometrical analysis of folded surfaces profiles;Aller;Tectonophysics,2004

3. Geodynamic evolution of a Cadomian arc region: the northern Ossa-Morena zone, Iberian Massif;Bandrés;Tectonophysics,2002

4. The northern Ossa Morena Cadomian batholith (Iberian Massif): magmatic arc origin and early evolution;Bandrés;International Journal Earth Sciences,2004

5. A new method for the geometrical classification of large data sets of folds;Bastida;Journal of Structural Geology,1993

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