Open AccessLa disolución de rocas evaporíticas : un importante factor geomorfológico en el Valle del Ebro
Author(s) -
Juan Miguel A. Mandado Collado,
J. Rodríguez Vidal,
J. M. Tena
Publication year - 2013
Publication title -
cuadernos de investigación geográfica
Language(s) - English
Resource type - Journals
eISSN - 1697-9540
pISSN - 0211-6820
DOI - 10.18172/cig.931
Subject(s) - geology , anhydrite , gypsum , geomorphology , dome (geology) , geochemistry , humanities , art , paleontology
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.
Accelerating Research
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom
Address
John Eccles HouseRobert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom