Mineralogía y génesis de los filosilicatos del "Trias manchego" bajo la corteza neógena

• Autores: A. Córdoba Pardo, Anselmo Acosta Echevarría
• Localización: Boletín de la Sociedad Española de Mineralogía, ISSN 0210-6558, Vol. 15, Nº. 1, 1992, págs. 112-116
• Idioma: español
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• Resumen

  • In this paper a mineralogical and genetic study of clay minerals of Triassic sediments covered by Neogen rock at La Mancha (Ciudad Real) is being carried out. Most minerals (illite, kaolinite, smectite and interestratifield are part of the sediment as detritic products, another one mineral (paligorskite) is neoformed, and the rest, of them (interstratifield and clorite are origined by transformation.