Yacimientos de vertebrados en los materiales Paleógenos de la zona de Ulldemolins y Conca de Barbera, (Cuenca del Ebro, Tarragona): significado Estratigräfico
The Ulldemolins Complex, which is characterized by different lithotypes, contains several types of fossil remains such as ostracoda, gastropoda, charophyta and micromammalia. This fossil association suggests that the Complex was deposited during the Culsian-Bartonlan time span. The outcrops located...
| Autores: | ; ; ; ; |
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| Tipo de documento: | Artículo |
| Fecha de publicación: | 1994 |
| País: | España |
| Institución: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Lenguaje: | Español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/13834 |
| Acceso en línea: | http://hdl.handle.net/10272/13834 |
| Nivel de acceso: | Acceso abierto |
| Palabra clave: | Micromammalia Charophyta Marine fossil remains Paleogene Ebro basin Tarragona |
| _version_ | 1878735430793297920 |
|---|---|
| author | Colombo Piñol, Ferrán |
| author2 | Moya, S. Checa, L. Agustí, J. Köhler, M. |
| author2_role | author author author author |
| author_browse | Agustí, J. Checa, L. Colombo Piñol, Ferrán Köhler, M. Moya, S. |
| author_facet | Colombo Piñol, Ferrán Moya, S. Checa, L. Agustí, J. Köhler, M. |
| author_role | author |
| collection | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| description | The Ulldemolins Complex, which is characterized by different lithotypes, contains several types of fossil remains such as ostracoda, gastropoda, charophyta and micromammalia. This fossil association suggests that the Complex was deposited during the Culsian-Bartonlan time span. The outcrops located near the Ulldemolins village, which are characterized by mammalian remains, suggest that lower levels of Ulldemolins Complex were deposited during the Culslan time span. The outcrops located in the Conca d e Barberà area Indicate that the levels of the Montblanc Formation were deposited during the Bartonian-Pnabonian time span. The outcrops located near Vimbodi area suggest that the levels of Biancafort Fm were deposited during Lower Oligocene times |
| eu_rights_str_mv | openAccess |
| format | article |
| id | ES_7c8e2e9b3fe9fb6298ff7ca3a09b3122 |
| institution | Universidad de Huelva (UHU) |
| instname_str | Universidad de Huelva (UHU) |
| language | spa |
| network_acronym_str | ES |
| network_name_str | España |
| oai_identifier_str | oai:ariasmontano.uhu.es:10272/13834 |
| publishDate | 1994 |
| publishDateSort | 1994 |
| publisher | Sociedad Geológica de España |
| publisherStr | Sociedad Geológica de España |
| reponame_str | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| spelling | Yacimientos de vertebrados en los materiales Paleógenos de la zona de Ulldemolins y Conca de Barbera, (Cuenca del Ebro, Tarragona): significado Estratigräfico Vertebrate fossil remains in the Paleogene of the Conca de Barbera and Ulldemolins areas, (Ebro Basin, Tarragona): stratigraphic Implications Colombo Piñol, Ferrán Moya, S. Checa, L. Agustí, J. Köhler, M. Micromammalia Charophyta Marine fossil remains Paleogene Ebro basin Tarragona The Ulldemolins Complex, which is characterized by different lithotypes, contains several types of fossil remains such as ostracoda, gastropoda, charophyta and micromammalia. This fossil association suggests that the Complex was deposited during the Culsian-Bartonlan time span. The outcrops located near the Ulldemolins village, which are characterized by mammalian remains, suggest that lower levels of Ulldemolins Complex were deposited during the Culslan time span. The outcrops located in the Conca d e Barberà area Indicate that the levels of the Montblanc Formation were deposited during the Bartonian-Pnabonian time span. The outcrops located near Vimbodi area suggest that the levels of Biancafort Fm were deposited during Lower Oligocene times Sociedad Geológica de España http://hdl.handle.net/10272/13834 |
| spellingShingle | Yacimientos de vertebrados en los materiales Paleógenos de la zona de Ulldemolins y Conca de Barbera, (Cuenca del Ebro, Tarragona): significado Estratigräfico Colombo Piñol, Ferrán Micromammalia Charophyta Marine fossil remains Paleogene Ebro basin Tarragona |
| title | Yacimientos de vertebrados en los materiales Paleógenos de la zona de Ulldemolins y Conca de Barbera, (Cuenca del Ebro, Tarragona): significado Estratigräfico |
| title_full | Yacimientos de vertebrados en los materiales Paleógenos de la zona de Ulldemolins y Conca de Barbera, (Cuenca del Ebro, Tarragona): significado Estratigräfico |
| title_fullStr | Yacimientos de vertebrados en los materiales Paleógenos de la zona de Ulldemolins y Conca de Barbera, (Cuenca del Ebro, Tarragona): significado Estratigräfico |
| title_full_unstemmed | Yacimientos de vertebrados en los materiales Paleógenos de la zona de Ulldemolins y Conca de Barbera, (Cuenca del Ebro, Tarragona): significado Estratigräfico |
| title_short | Yacimientos de vertebrados en los materiales Paleógenos de la zona de Ulldemolins y Conca de Barbera, (Cuenca del Ebro, Tarragona): significado Estratigräfico |
| title_sort | Yacimientos de vertebrados en los materiales Paleógenos de la zona de Ulldemolins y Conca de Barbera, (Cuenca del Ebro, Tarragona): significado Estratigräfico |
| topic | Micromammalia Charophyta Marine fossil remains Paleogene Ebro basin Tarragona |
| topic_facet | Micromammalia Charophyta Marine fossil remains Paleogene Ebro basin Tarragona |
| url | http://hdl.handle.net/10272/13834 |