Publication: El Trías de Alcázar de San Juan (Región de La Mancha).
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1977
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Servicio de Publicaciones de la Universidad Complutense de Madrid
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Abstract
Se ha levantado una columna litoestratigráfica de detalle entre Alcázar de San Juan y Campo dc Criptana, distinguiéndose seis unidades que en conjunto pasan de tener neto carácter detrítico en la base a facies evaporíticas en el techo. La potencia total es de 140 a 180 metros. Se definen los caracteres petrológicos y sedimentológicos, comparándose sus facies con los materiales triásicos de la Cordillera Ibérica y de la zona prebética.
Six units have been differentiated in a detailed litho-stratigraphic column between Alcázar de San Juan and Campo de Criptana. These six units present a clear detrital character at the base which changes lo evaporitic facies toward Ihe top. The petrological and sedimentological characteristics are defined, comparing their facies with Ihe Triassic materials of the Iberian Range and Ihe prebetie zone.
Six units have been differentiated in a detailed litho-stratigraphic column between Alcázar de San Juan and Campo de Criptana. These six units present a clear detrital character at the base which changes lo evaporitic facies toward Ihe top. The petrological and sedimentological characteristics are defined, comparing their facies with Ihe Triassic materials of the Iberian Range and Ihe prebetie zone.