Climatic vs. tectonic signals in a continental extensional basin (Teruel, NE Spain) from stable isotope (δ18O) and sequence stratigraphical evolution
Alluvial fans and shallow carbonate lakes interfered in the Teruel half-graben during the Late Miocene–Pliocene. Tectonic influence is recorded in alluvial and lacustrine–palustrine successions, with long-term climate changes being recorded in detail in the isotopic signatures of carbonates. Episode...
| Autores: | , , , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 2014 |
| País: | España |
| Institución: | Universidad Complutense de Madrid (UCM) |
| Repositorio: | Docta Complutense |
| Idioma: | inglés |
| OAI Identifier: | oai:docta.ucm.es:20.500.14352/116437 |
| Acceso en línea: | https://hdl.handle.net/20.500.14352/116437 |
| Access Level: | acceso abierto |
| Palabra clave: | 551.78(460.226) Geología estratigráfica 2506.19 Estratigrafía |
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Climatic vs. tectonic signals in a continental extensional basin (Teruel, NE Spain) from stable isotope (δ18O) and sequence stratigraphical evolution Ezquerro Ruiz, Lope Luzón Aguado, Aránzazu Navarro, Marta Liesa, Carlos L. Simón, J.L. 551.78(460.226) Geología estratigráfica 2506.19 Estratigrafía Alluvial fans and shallow carbonate lakes interfered in the Teruel half-graben during the Late Miocene–Pliocene. Tectonic influence is recorded in alluvial and lacustrine–palustrine successions, with long-term climate changes being recorded in detail in the isotopic signatures of carbonates. Episodes of tectonic activity induced alluvial fan progradation and lake retraction in the whole basin. Three lacustrine stages have been identified, which support the idea that climate also exerted an important control on sedimentation. The transition between stages 1 and 2 occurred during a tectonically calm episode due to an increase in aridity in the Early Turolian; small fans with source areas next to the lake margin prograded, inducing lake-shore retraction. The transition from stage 2 to 3 was caused by the superimposition of increasing tectonic activity and aridity effects. Our study demonstrates that discrimination of allogenic factors controlling sedimentation in continental closed basins is possible using sequence stratigraphy in combination with other techniques such as geochemistry of carbonates. Wiley https://hdl.handle.net/20.500.14352/116437 |
| title |
Climatic vs. tectonic signals in a continental extensional basin (Teruel, NE Spain) from stable isotope (δ18O) and sequence stratigraphical evolution |
| spellingShingle |
Climatic vs. tectonic signals in a continental extensional basin (Teruel, NE Spain) from stable isotope (δ18O) and sequence stratigraphical evolution Ezquerro Ruiz, Lope 551.78(460.226) Geología estratigráfica 2506.19 Estratigrafía |
| title_short |
Climatic vs. tectonic signals in a continental extensional basin (Teruel, NE Spain) from stable isotope (δ18O) and sequence stratigraphical evolution |
| title_full |
Climatic vs. tectonic signals in a continental extensional basin (Teruel, NE Spain) from stable isotope (δ18O) and sequence stratigraphical evolution |
| title_fullStr |
Climatic vs. tectonic signals in a continental extensional basin (Teruel, NE Spain) from stable isotope (δ18O) and sequence stratigraphical evolution |
| title_full_unstemmed |
Climatic vs. tectonic signals in a continental extensional basin (Teruel, NE Spain) from stable isotope (δ18O) and sequence stratigraphical evolution |
| title_sort |
Climatic vs. tectonic signals in a continental extensional basin (Teruel, NE Spain) from stable isotope (δ18O) and sequence stratigraphical evolution |
| author |
Ezquerro Ruiz, Lope |
| author_facet |
Ezquerro Ruiz, Lope Luzón Aguado, Aránzazu Navarro, Marta Liesa, Carlos L. Simón, J.L. |
| author_role |
author |
| author2 |
Luzón Aguado, Aránzazu Navarro, Marta Liesa, Carlos L. Simón, J.L. |
| author2_role |
author author author author |
| topic |
551.78(460.226) Geología estratigráfica 2506.19 Estratigrafía |
| topic_facet |
551.78(460.226) Geología estratigráfica 2506.19 Estratigrafía |
| description |
Alluvial fans and shallow carbonate lakes interfered in the Teruel half-graben during the Late Miocene–Pliocene. Tectonic influence is recorded in alluvial and lacustrine–palustrine successions, with long-term climate changes being recorded in detail in the isotopic signatures of carbonates. Episodes of tectonic activity induced alluvial fan progradation and lake retraction in the whole basin. Three lacustrine stages have been identified, which support the idea that climate also exerted an important control on sedimentation. The transition between stages 1 and 2 occurred during a tectonically calm episode due to an increase in aridity in the Early Turolian; small fans with source areas next to the lake margin prograded, inducing lake-shore retraction. The transition from stage 2 to 3 was caused by the superimposition of increasing tectonic activity and aridity effects. Our study demonstrates that discrimination of allogenic factors controlling sedimentation in continental closed basins is possible using sequence stratigraphy in combination with other techniques such as geochemistry of carbonates. |
| publishDate |
2014 |
| format |
article |
| url |
https://hdl.handle.net/20.500.14352/116437 |
| language |
eng |
| eu_rights_str_mv |
openAccess |
| publisher |
Wiley |
| institution |
Universidad Complutense de Madrid (UCM) |
| collection |
Docta Complutense |
| reponame_str |
Docta Complutense |
| instname_str |
Universidad Complutense de Madrid (UCM) |
| _version_ |
1878440176456302593 |
| publishDateSort |
2014 |
| author_browse |
Ezquerro Ruiz, Lope Liesa, Carlos L. Luzón Aguado, Aránzazu Navarro, Marta Simón, J.L. |
| publisherStr |
Wiley |
| score |
6,9303427 |