Mineralogía de los materiales de la Formación de La Viñuela (Cordilleras Béticas)
DOI:
https://doi.org/10.3989/egeol.84405-6668Keywords:
Clay minerals, zeolites, diagenesis, Tertiary, Cordilleras Béticas.Abstract
Mineralogy of several samples from the Viñuela Formation,Lower Burdigalian (Vélez Málaga, Cordilleras Béticas), has been studied. Materials are composed of abundant microfauna. and pebbles of micaschits, quartzites and other materials, from the Alpujárrides and Maláguides Nappes, cemented by a micritic matrix . Most samples contain zeolites (clinoptilolite, mordenite and analcime), and illite chlorite, interstratified clay minerals, montmorillonite and opal C-T. A diagenetic genesis for zeolites is suggested.
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Published
1984-12-30
How to Cite
Galán, E., González, J. M., Fernández Nieto, C., & Barceló, G. (1984). Mineralogía de los materiales de la Formación de La Viñuela (Cordilleras Béticas). Estudios Geológicos, 40(5-6), 259–268. https://doi.org/10.3989/egeol.84405-6668
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