000086131 001__ 86131
000086131 005__ 20230914083234.0
000086131 0247_ $$2doi$$a10.1016/j.jsg.2018.11.011
000086131 0248_ $$2sideral$$a110426
000086131 037__ $$aART-2019-110426
000086131 041__ $$aeng
000086131 100__ $$0(orcid)0000-0002-9130-117X$$aLiesa, C.L.$$uUniversidad de Zaragoza
000086131 245__ $$aStress evolution and structural inheritance controlling an intracontinental extensional basin: The central-northern sector of the Neogene Teruel Basin
000086131 260__ $$c2019
000086131 5060_ $$aAccess copy available to the general public$$fUnrestricted
000086131 5203_ $$aThe Teruel Basin is a NNE-SSW trending intracontinental extensional basin located in central-eastern Iberia. It is asymmetrically bounded to the east by a major fault zone, but intrabasinal faults with diverse orientation (NNE-SSW to NE-SW, E-W, or NW-SE) also appear. Offsets of the successive sedimentary units and of two planation surfaces reveal that tectonic activity initiated at the border faults, while intrabasinal ones mainly developed in a later stage. Fractures on a map scale show a prevailing N-S strike in Neogene synrift rocks, while a dense network made of four main fracture sets (NE-SW, E-W to ESE-WNW, N-S and NNW-SSE), likely inherited from Mesozoic rifting stages, is observed in pre-rift units. The results of palaeostress analyses indicate an overall predominance of s3 directions around E-W, although two stress episodes have been distinguished during the Late Miocene-Pleistocene: (i) triaxial extension with s3 E-W; (ii) almost ‘radial’ extension (s1 vertical, s2 ˜ s3) with a somehow prevailing s3 ENE-WSW. A scenario in which the evolving extensional stress field was able to gradually activate major basement structures with different orientation, inherited from previous tectonic events, is proposed as responsible for the evolution and overall pattern of both the eastern active margin and central parts of the central-northern sector of the Teruel Basin.
000086131 536__ $$9info:eu-repo/grantAgreement/ES/DGA/E32-17R$$9info:eu-repo/grantAgreement/ES/MINECO-FEDER/CGL2012-35662$$9info:eu-repo/grantAgreement/ES/UZ/UZ2017-CIE-01
000086131 540__ $$9info:eu-repo/semantics/openAccess$$aby-nc-nd$$uhttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
000086131 590__ $$a2.836$$b2019
000086131 591__ $$aGEOSCIENCES, MULTIDISCIPLINARY$$b65 / 198 = 0.328$$c2019$$dQ2$$eT1
000086131 592__ $$a1.431$$b2019
000086131 593__ $$aGeology$$c2019$$dQ1
000086131 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/acceptedVersion
000086131 700__ $$0(orcid)0000-0003-1412-5245$$aSimón, J.L.$$uUniversidad de Zaragoza
000086131 700__ $$0(orcid)0000-0003-0900-1440$$aEzquerro, L.
000086131 700__ $$0(orcid)0000-0001-5091-9398$$aArlegui, L.E.$$uUniversidad de Zaragoza
000086131 700__ $$0(orcid)0000-0002-8929-9429$$aLuzón, A.$$uUniversidad de Zaragoza
000086131 7102_ $$12000$$2428$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Geodinámica Interna
000086131 7102_ $$12000$$2280$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Estratigrafía
000086131 773__ $$g118 (2019), 362-376$$pJ. struct. geol.$$tJournal of Structural Geology$$x0191-8141
000086131 8564_ $$s1010635$$uhttps://zaguan.unizar.es/record/86131/files/texto_completo.pdf$$yPostprint
000086131 8564_ $$s197990$$uhttps://zaguan.unizar.es/record/86131/files/texto_completo.jpg?subformat=icon$$xicon$$yPostprint
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000086131 951__ $$a2023-09-13-10:45:20
000086131 980__ $$aARTICLE