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Caracterización de la unidad Conglomerados de Valdemeca en la transición Pérmico-Triásico de la Cordillera Ibérica centro- oriental.

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De la Horra, R. and López Gómez, José and Arche, Alfredo (2005) Caracterización de la unidad Conglomerados de Valdemeca en la transición Pérmico-Triásico de la Cordillera Ibérica centro- oriental. Geotemas, 8 . pp. 141-145. ISSN 1576-5172

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Abstract

The Valdemeca Conglomerates unit is here described as the basal part of the Late Permian-Early Triassic sedimentary cycle in the central-eastern part of the Iberian Ranges, equivalent to the upper part of the Hoz de Callo Conglomerates Formation of the classic Molina de Aragón area. It is interpreted as braided river deposits with paleocurrents parallel to the basin axis. The identification in this new area represents the expand of the sedimentation realm of this cycle to the SE of the Iberian Ranges.


Item Type:Article
Uncontrolled Keywords:Permian, Triassic, Buntsandstein, Permian-Triassic Boundary, Iberian Ranges, Valdemeca Conglomerates
Subjects:Sciences > Geology > Stratigraphic geology
ID Code:60670
Deposited On:28 May 2020 11:21
Last Modified:28 May 2020 11:59

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