Estudio del Terciario marino de la sierra del Mugrón (Prov. Albncete y Valencia)
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1974
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Instituto Jaime Almera, Consejo Superior de Investigaciones Científicas Universidad de Barcelona, Facultad de Geología
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Abstract
Los sedimentos miocenos que constituyen la sierra del Mugrón ofrecen un buen ejemplo de sedimentación marina en facies litoral. Las observaciones estratigráficas y petrológicas realizadas, así como los datos aportados por la micro y macropaleontología, permiten interpretar las condiciones de depósito de estos materiales. La sedimentación tuvo lugar en un medio de plataforma continental interna, muy ligada en un principio a procesos tectónicos regionales, presentando con posterioridad un gran desarrollo de organismos coloniales.
The Miocene sediments of sierra del Mugron give us a good example of marine sedimentation in littoral facies. The stratigraphic observatior~s effectued, the petrologic characteristics of these materials and their classification, are analyzed in this paper. The set of these dates, with the help of macro and micropaleontologic criteries permits to interpret the conditions of deposition. It is concluded this deposition occurred in the internal continental plattform, in relation with regional tectonic process and a great development of colonial organisms.
The Miocene sediments of sierra del Mugron give us a good example of marine sedimentation in littoral facies. The stratigraphic observatior~s effectued, the petrologic characteristics of these materials and their classification, are analyzed in this paper. The set of these dates, with the help of macro and micropaleontologic criteries permits to interpret the conditions of deposition. It is concluded this deposition occurred in the internal continental plattform, in relation with regional tectonic process and a great development of colonial organisms.