Evolución tectosedimentaria de la Fm. Blesa (Cretàcico Inferior) en el entorno del yacimiento de vertebrados de La Cantalera (Josa, Teruel)
Geological mapping and fades analysis of the Jurassic-Lower Cretaceous units located around the La Cantalera fossil site (Josa locality, Teruel Province, NE Spain), has allowed a precise reconstruction of a continental sedimentary basin developed around the Hauterivian-Barremian turnover. The first...
| Autores: | , , |
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| Tipo de documento: | artigo |
| Data de publicação: | 2003 |
| País: | España |
| Recursos: | Universidad de Huelva (UHU) |
| Repositório: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | espanhol |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/8988 |
| Acesso em linha: | http://hdl.handle.net/10272/8988 |
| Access Level: | Acceso aberto |
| Palavra-chave: | Iberian Chain Synsedimentary tectonics Alluvial fans Vertebrates |
| Resumo: | Geological mapping and fades analysis of the Jurassic-Lower Cretaceous units located around the La Cantalera fossil site (Josa locality, Teruel Province, NE Spain), has allowed a precise reconstruction of a continental sedimentary basin developed around the Hauterivian-Barremian turnover. The first stage of evolution of the basin was controlled by intense normal fault activity and resulted in the formation of an isolated basin, surrounded by limestone-marly relief. The existence of a non-permanent water marshy area, with an important vegetated area, explain the abundance and diversity of the fossil remains in the studied locality |
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