Climatic vs. tectonic signals in a continental extensional basin (Teruel, NE Spain) from stable isotope ( 18O) and sequence stratigraphical evolution

Ezquerro, L. (Universidad de Zaragoza) ; Luzón, A. (Universidad de Zaragoza) ; Navarro, M. ; Liesa, C. L. (Universidad de Zaragoza) ; Simón,J. L. (Universidad de Zaragoza)

Resumen: 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.

Idioma: Inglés

DOI: 10.1111/ter.12101

Año: 2014

Publicado en: TERRA NOVA 26, 5 (2014), 337-346
ISSN: 0954-4879

Factor impacto JCR: 2.639 (2014)

Categ. JCR: GEOSCIENCES, MULTIDISCIPLINARY rank: 40 / 175 = 0.229 (2014) - Q1 - T1

Financiación: info:eu-repo/grantAgreement/ES/MINECO/CGL2009-13390
Financiación: info:eu-repo/grantAgreement/ES/MINECO/CGL2012-35662

Tipo y forma: Artículo (PrePrint)

Área (Departamento): Área Geodinámica Interna (Dpto. Ciencias de la Tierra)
Área (Departamento): Área Estratigrafía (Dpto. Ciencias de la Tierra)