Tectonic evolution around the Sierra de Arcos thrust (Ariño, northeaster Iberian Chain)

Authors

  • Daniel Ruiz Blasco Departamento de Ciencias de la Tierra, Universidad de Zaragoza
  • Teresa Román Berdiel Departamento de Ciencias de la Tierra, Grupo Geotransfer-IUCA, Universidad de Zaragoza

DOI:

https://doi.org/10.55407/geogaceta100902

Keywords:

Iberian Chain, Alpine Orogeny, tectonic structures, stress field, anisotropy

Abstract

The Ariño sector of the Aragonese Branch of the Iberian Chain (Oliete basin) shows a set of macrostructures resulting from its tectonic evolution: NNW-SSE, E-W and NW-SE trending folds, and a plurikilometricthrust (Sierra de Arcos thrust) detached on the Upper Triassic evaporites. Mesostrutures include normal faults forming conjugate systems, stylolytic peaks with two main preferred directions and cleavage planes associated with normal and overturned limbs in the Upper Triassic. The analysis of these structures allows to propose two different hypotheses about the tectonic evolution of this sector of the Iberian Chain during the Cenozoic. The first one deals with several compressional episodes with differently oriented stress axis that generated the tectonic structures present in the study arena. The second one is focused in the interpretation of an only N-NNE oriented compression, the different orientation of the structures found resulting from the orientation anisotropy of structural features, resulting from the previous basinal evolution of the area.

References

Allmendinger, R. W., Cardozo, N. C. y Fisher, D. (2013). Structural Geology Algorithms: Vectors & Tensors: Cambridge, Englad, Cambridge University Press, 289 pp.

Anderson, E. M. (1951). The dynamics of faulting and dyke formation with application to Britain. Oliver & Boyd Ed. Reprinted of the revised second edition (1963), 206 pp.

Aurell, M., Bádenas, B., Canudo, J.I. y Casas, A. (2017). Guía de geología y paleontología del Parque Cultural del Río Martín, Edición Renovada. Asociación Parque Cultural del Río Martín, Ariño, 151 pp.

Aurell, M., Soria, A.R., Bádenas, B., Liesa, C.L., Canudo, J.I., Gasca, J.M., Moreno-Azanza, M., Medrano-Aguado, E. y Meléndez, A. (2018). Journal of Iberian Geology 44(2), 285-308. https://doi.org/10.1007/s41513-018-0057-3

Bordonaba, A. P. y Aurel M. (2001). Revista de la Sociedad Geológica de España 14(1-2), 135-146.

Bordonaba, A. P., Aurel M. y Casas, A. (1999). Geogaceta 25, 43-46. Casas, A. M., Cortes, A. L., Liesa, C. L., Meléndez, A. y Soria, A. R. (1997). Cuadernos de geología ibérica 23, 243-268.

Delvene, G., Meléndez, G., Bello, J. y Pérez, I. (1997). Cuadernos de geología ibérica 23, 269-300.

Liesa, C.L. (2000). Fracturación y campos de esfuerzos compresivos alpinos en la Cordillera Ibérica y el NE peninsular. Tesis Doctoral, Universidad de Zaragoza, 760 pp.

Liesa, C.L., Casas, A. M. y Simón, J.L. (2018). Revista de la Sociedad Geológica de España, 31(2), 23-50.

Ríos, L.M., Beltrán, F.J., Lanaja, J.M. y Marín, F.J. (1981). Mapa Geológico de España E. 1:50.000, Hoja 467 Muniesa.

Simón, J.L. y Liesa, C.L. (2011). Geological Society of London, Special Publications 349, 77-79. https://doi.org/10.1144/SP349.5

Soria, A.R., Vennin, E. y Meléndez, A. (1992). Revista de la Sociedad Geológica de España 8(1-2), 47-61.

Published

2024-06-29

How to Cite

Ruiz Blasco, D., & Román Berdiel, T. (2024). Tectonic evolution around the Sierra de Arcos thrust (Ariño, northeaster Iberian Chain). GEOGACETA, 75, 47–50. https://doi.org/10.55407/geogaceta100902

Issue

Section

Artículos