The Permian and Triassic of the central Cantabrian Mountains (Eastern Asturias- Western Cantabria, N Spain)
This field trip shows new data based on recent work by the organizing research team. These data show a new stratigraphic chart based on precise ages of each defined unit, a reinterpretation of their sedimentary evolution and the development of a new Variscan-Alpine tectono-sedimentary framework. Fur...
| Autores: | , , , , , , , , , , , , , , , |
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| Tipo de recurso: | libro |
| Fecha de publicación: | 2022 |
| País: | España |
| Institución: | Universidad de Oviedo (UNIOVI) |
| Repositorio: | RUO. Repositorio Institucional de la Universidad de Oviedo |
| Idioma: | inglés |
| OAI Identifier: | oai:digibuo.uniovi.es:10651/69322 |
| Acceso en línea: | https://hdl.handle.net/10651/69322 |
| Access Level: | acceso abierto |
| Palabra clave: | Cantabrian Mountains Alpine cycle Structural geology |
| Sumario: | This field trip shows new data based on recent work by the organizing research team. These data show a new stratigraphic chart based on precise ages of each defined unit, a reinterpretation of their sedimentary evolution and the development of a new Variscan-Alpine tectono-sedimentary framework. Furthermore, the new data reveal for the time a similar geodynamic evolution across the Pyrenean-Cantabrian basins at the end of the Variscan cycle and even with those formed within Western and Central Europe during the early-middle Permian. This new obtained information is based on a multidisciplinary work, including geological mapping, sedimentology, mineralogy, petrology of volcanic rocks and new paleontological data. |
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