Los materiales Ordovícicos en el arca de Retuerta del Bullaque, sinclinal de Navas de Estena (Ciudad Real)
DOI:
https://doi.org/10.3989/egeol.89455-6511Keywords:
Ordovician, Llanvim, Dobrotivian, new localities, Hesperian Massif, Montes de Toledo, Ciudad Real, SpainAbstract
This paper deals with the stratigraphy of Ordovician sediments, mainly those of the Llanvirn Dobrotivian (Llandeilo) in the Retuerta del Bullaque area (Ciudad Real). The study is based on that originate from twenty four outcrops distributed throughout the «Tristani beds» Most exposures are new to scientific literature. Cartography of this area is also presented.
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