Caracterización de la unidad Conglomerados de Valdemeca en la transición Pérmico-Triásico de la Cordillera Ibérica centro- oriental.
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 interprete...
| Authors: | , , |
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| Format: | article |
| Publication Date: | 2005 |
| Country: | España |
| Institution: | Universidad Complutense de Madrid (UCM) |
| Repository: | Docta Complutense |
| Language: | Spanish |
| OAI Identifier: | oai:docta.ucm.es:20.500.14352/52503 |
| Online Access: | https://hdl.handle.net/20.500.14352/52503 |
| Access Level: | Open access |
| Keyword: | 551.7 Permian Triassic Buntsandstein Permian-Triassic Boundary Iberian Ranges Valdemeca Conglomerates Geología estratigráfica 2506.19 Estratigrafía |
| Summary: | 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. |
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