José María Amigó Descarrega, Joaquín Bastida Cuairan, J. V. Clausell Borja, Ángel M. López Buendía
The mineralógicaI composition and FWHM values for 001 and 002 of kaolinite and ¡Hite in the <40 pm fraction of sands and shales of the Utrillas Fm in Algarra (Cuenca) show relevant features of the mineralogical assemblages and genetic systemas as diagenetic probable processes involved in the origin of kaolins.
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