Geological interpretation of two virtual outcrops of deformed Palaeozoic rocks (NW Iberian Peninsula) using 3D stereo VDT in a computer assisted virtual environment (CAVE™)

Author:

Martín Santiago,Uzkeda HodeiORCID,Poblet Josep,Bulnes Mayte

Funder

Ministerio de Economía y Competitividad

European Fund for Regional Development

Repsol Exploración S.A.

Publisher

Springer Science and Business Media LLC

Subject

Stratigraphy,Geology

Reference74 articles.

1. Aller, J., Álvarez-Marrón, J., Bastida, F., Bulnes, M., Heredia, N., Marcos, A., et al. (2004). Estructura, deformación y metamorfismo (Zona Cantábrica). In J. A. Vera (Ed.), Geología de España (pp. 42–49). Madrid: Sociedad Geológica de España-Instituto Geológico y Minero de España.

2. Alonso, J. L., Álvarez-Marrón, J., Aller, J., Bastida, F., Farias, P., Marcos, A., et al. (1992). Estructura de la Zona Cantábrica. In J. G. Gutiérrez Maco, J. Saavedra, & I. Rábano (Eds.), Paleozoico Inferior de Ibero-América (pp. 423–434). Badajoz: Universidad de Extremadura.

3. Alonso, J. L., Marcos, A., & Suárez-Rodríguez, A. (2009). Paleogeographic inversion resulting from large out of sequence breaching thrusts: the León Fault (Cantabrian Zone, NW Iberia). A new picture of the external Variscan thrust belt in the Ibero-Armorican Arc. Geologica Acta,7(4), 451–473.

4. Alonso, J. L., & Teixell, A. (1992). Forelimb deformation in some natural examples of fault-propagation folds. In K. McClay (Ed.), Thrust Tectonics (pp. 175–180). London: Chapman, & Hall.

5. Banerjee, S., & Mitra, S. (2004). Remote surface mapping using orthophotos and geologic maps draped over digital elevation models: Application the Sheep Mountain anticline, Wyoming. AAPG Bulletin,88(9), 1227–1237.

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