La cobertera paleozoica posthercínica en el Oriente de Asturias
The discovery of plant fragments in the basal marine quartzites of the post-Hercynian cover at the locality of Mestas de Con (Asturias), which have been determined as Stephanian C or Autunian, allows dating the end of the Hercynian Orogenesis in the eastern Cantabrian Mountains as restricted to the...
| Autores: | , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1991 |
| País: | España |
| Institución: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/18069 |
| Acceso en línea: | http://hdl.handle.net/10272/18069 |
| Access Level: | acceso abierto |
| Palabra clave: | Asturias Cantabrian Mountains Stephanian Permian |
| Sumario: | The discovery of plant fragments in the basal marine quartzites of the post-Hercynian cover at the locality of Mestas de Con (Asturias), which have been determined as Stephanian C or Autunian, allows dating the end of the Hercynian Orogenesis in the eastern Cantabrian Mountains as restricted to the time interval between late Stephanian B and Stephanian C-Autunian |
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