000148163 001__ 148163
000148163 005__ 20250115151522.0
000148163 0247_ $$2doi$$a10.1111/ter.12101
000148163 0248_ $$2sideral$$a87699
000148163 037__ $$aART-2014-87699
000148163 041__ $$aeng
000148163 100__ $$0(orcid)0000-0003-0900-1440$$aEzquerro, L.$$uUniversidad de Zaragoza
000148163 245__ $$aClimatic vs. tectonic signals in a continental extensional basin (Teruel, NE Spain) from stable isotope ( 18O) and sequence stratigraphical evolution
000148163 260__ $$c2014
000148163 5060_ $$aAccess copy available to the general public$$fUnrestricted
000148163 5203_ $$aAlluvial 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.
000148163 536__ $$9info:eu-repo/grantAgreement/ES/MINECO/CGL2009-13390$$9info:eu-repo/grantAgreement/ES/MINECO/CGL2012-35662
000148163 540__ $$9info:eu-repo/semantics/openAccess$$aAll rights reserved$$uhttp://www.europeana.eu/rights/rr-f/
000148163 590__ $$a2.639$$b2014
000148163 591__ $$aGEOSCIENCES, MULTIDISCIPLINARY$$b40 / 175 = 0.229$$c2014$$dQ1$$eT1
000148163 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/submittedVersion
000148163 700__ $$0(orcid)0000-0002-8929-9429$$aLuzón, A.$$uUniversidad de Zaragoza
000148163 700__ $$0(orcid)0000-0001-7702-9619$$aNavarro, M.
000148163 700__ $$0(orcid)0000-0002-9130-117X$$aLiesa, C. L.$$uUniversidad de Zaragoza
000148163 700__ $$0(orcid)0000-0003-1412-5245$$aSimón,J. L.$$uUniversidad de Zaragoza
000148163 7102_ $$12000$$2428$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Geodinámica Interna
000148163 7102_ $$12000$$2280$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Estratigrafía
000148163 773__ $$g26, 5 (2014), 337-346$$pTerra Nova$$tTERRA NOVA$$x0954-4879
000148163 8564_ $$s2385845$$uhttps://zaguan.unizar.es/record/148163/files/texto_completo.pdf$$yVersión publicada
000148163 8564_ $$s764615$$uhttps://zaguan.unizar.es/record/148163/files/texto_completo.jpg?subformat=icon$$xicon$$yVersión publicada
000148163 909CO $$ooai:zaguan.unizar.es:148163$$particulos$$pdriver
000148163 951__ $$a2025-01-15-15:14:42
000148163 980__ $$aARTICLE