La disolución de rocas evaporíticas : un importante factor geomorfológico en el Valle del Ebro

Authors

  • J. Mandado Universidad de Zaragoza
  • J. Rodríguez Vidal Universidad de Zaragoza
  • J. M. Tena Universidad de Zaragoza

DOI:

https://doi.org/10.18172/cig.931

Abstract

The analysis of different physical-chemical factors for the solubilitation of the system gypsum-anhydrite remark the significance of textures and contents of NaCl in solutíon. Geomorphologíc processes such as the escarp and the dome of Remolinos or the depressions in El Castellar are effects of disolution phenomena for evaporitic materials in the Ebro Valley.

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Published

21-05-2013

How to Cite

1.
Mandado J, Rodríguez Vidal J, Tena JM. La disolución de rocas evaporíticas : un importante factor geomorfológico en el Valle del Ebro. CIG [Internet]. 2013 May 21 [cited 2024 Apr. 13];10:139-48. Available from: https://publicaciones.unirioja.es/ojs/index.php/cig/article/view/931