Las facies Muschelkalk de Henarejos (Cuenca): sedimentología y fauna del tramo superior.
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Publication date
1987
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Editorial Complutense
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Abstract
Se estudian las características estratigráficas y así como las faunas de bivalvos y ammonoideos que aparecen en el tramo superior carbonatado de Facies Muschelkalk en el afloramientode Henarejos (provincia de Cuenca) (fig. 1). Se ha levantado la columna estratigráfica donde se muestran las citadas características (fig. 2).La interpretación sedimentaria se realiza a partir de asociaciones de facies (Hg. 4), que quedan incluidas en diferentes subambientes de llanura mareal (fig. 3), siendo comparadas con las secuencias tipo «shallowing» de JAMES (1976).
The stratigrafic and sedimentological caracteristies of the upper carbonatie level of the Muschelkalk Facies of Henarejos, Cuenca Province (fig. 1) are studied as well as their Bivalv and Ammonoid faunas. A synthetic section (fig. 2) is also presented here The sedimentological interpretation is based on typical facies associations (fig. 4) interpreted as different tidal fiat subenvironments (fig. 3) comparable to the shallowing upwards sequences of JAMES (1976).
The stratigrafic and sedimentological caracteristies of the upper carbonatie level of the Muschelkalk Facies of Henarejos, Cuenca Province (fig. 1) are studied as well as their Bivalv and Ammonoid faunas. A synthetic section (fig. 2) is also presented here The sedimentological interpretation is based on typical facies associations (fig. 4) interpreted as different tidal fiat subenvironments (fig. 3) comparable to the shallowing upwards sequences of JAMES (1976).