000118613 001__ 118613
000118613 005__ 20220921104420.0
000118613 0247_ $$2doi$$a10.1016/j.tecto.2019.05.014
000118613 0248_ $$2sideral$$a112591
000118613 037__ $$aART-2019-112591
000118613 041__ $$aeng
000118613 100__ $$aMarcén, Marcos$$uUniversidad de Zaragoza
000118613 245__ $$aStrain variations in a seismogenic normal fault (Baza Sub-basin, Betic Chain): Insights from magnetic fabrics (AMS)
000118613 260__ $$c2019
000118613 5060_ $$aAccess copy available to the general public$$fUnrestricted
000118613 5203_ $$aAMS and structural analysis are here applied to study the deformed zone associated with a large-scale, active normal fault in the central Betic Cordillera (Spain), namely the Baza fault system, to determine: i) the kinematics of structures and their relation with fault zone architecture and segmentation degree, ii) the correlation between deformational structures and the different types of magnetic fabrics and iii) the evolution of magnetic fabrics patterns, from sedimentary to shear-related, associated with normal faults. Five outcrops (969 samples) were analysed along the fault trace, which shows different degrees of segmentation along strike and strong localization of deformation along narrow fault zones. A first, main set of magnetic fabric data corroborates the normal kinematics of the Baza fault, showing magnetic lineations parallel to the dip-slip, transport direction. A second, secondary set of magnetic lineations, is parallel to the intersection lineation, and can be related to less intense deformation in the fault rocks. Furthermore, a detailed study (523 samples) of a trench excavated across the fault zone, where two fault splays tend to coalesce in a linkage relay zone indicates that i) lithology and distance to fault planes are two factors that control the development of extension-related magnetic fabrics in weakly deformed sediments, ii) the development of shear-related fabrics in fault zones entails the mechanical rotation of minerals, iii) different orientation of magnetic lineations are related to different intensity of bulk deformation and iv) magnetic lineation is useful to define local deviations of deformation axes produced by changes in the local extension direction (from fault-perpendicular to fault-parallel extension) in the linkage zone between adjacent fault splays.
000118613 536__ $$9info:eu-repo/grantAgreement/ES/MINECO/BES-2014-070167$$9info:eu-repo/grantAgreement/ES/MINECO/CGL2013-42670-P
000118613 540__ $$9info:eu-repo/semantics/openAccess$$aby-nc-nd$$uhttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
000118613 590__ $$a3.048$$b2019
000118613 591__ $$aGEOCHEMISTRY & GEOPHYSICS$$b31 / 84 = 0.369$$c2019$$dQ2$$eT2
000118613 592__ $$a1.529$$b2019
000118613 593__ $$aGeophysics$$c2019$$dQ1
000118613 593__ $$aEarth-Surface Processes$$c2019$$dQ1
000118613 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/acceptedVersion
000118613 700__ $$0(orcid)0000-0002-9743-8695$$aRomán-Berdiel, Teresa$$uUniversidad de Zaragoza
000118613 700__ $$0(orcid)0000-0003-3652-3527$$aCasas-Sainz, Antonio M.$$uUniversidad de Zaragoza
000118613 700__ $$0(orcid)0000-0002-1929-8850$$aSoto, Ruth
000118613 700__ $$0(orcid)0000-0003-1563-6434$$aOliva-Urcia, Belén
000118613 700__ $$aCastro, Julia
000118613 7102_ $$12000$$2428$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Geodinámica Interna
000118613 773__ $$g765 (2019), 64-82$$pTectonophysics$$tTectonophysics$$x0040-1951
000118613 8564_ $$s2287389$$uhttps://zaguan.unizar.es/record/118613/files/texto_completo.pdf$$yPostprint
000118613 8564_ $$s1015928$$uhttps://zaguan.unizar.es/record/118613/files/texto_completo.jpg?subformat=icon$$xicon$$yPostprint
000118613 909CO $$ooai:zaguan.unizar.es:118613$$particulos$$pdriver
000118613 951__ $$a2022-09-21-09:24:26
000118613 980__ $$aARTICLE