Los ciclos sedimentarios del Eoceno medio y superior en el sector NE de la depresión del Ebro (zona de Bergas-Vic). Caracterización de sus Iímites
In the middle and upper Eocene strata of the South Pyrenean foreland basin, three sedimentary cicles have been distinguished. These cycles are bounded by angular uncorfirmities, each cycle being related to the development of a particular thrust system. The stiking of the thrust systems is recorded b...
| Autores: | , |
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| Tipo de documento: | artigo |
| Data de publicação: | 1991 |
| 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:10272/18073 |
| Acesso em linha: | http://hdl.handle.net/10272/18073 |
| Access Level: | Acceso aberto |
| Palavra-chave: | Pyrenees Sedimentary cycles Unconformities Thrusting Eocene |
| Resumo: | In the middle and upper Eocene strata of the South Pyrenean foreland basin, three sedimentary cicles have been distinguished. These cycles are bounded by angular uncorfirmities, each cycle being related to the development of a particular thrust system. The stiking of the thrust systems is recorded by rhe angular uncorformities that bound the cycles |
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