000061287 001__ 61287
000061287 005__ 20171024120426.0
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000061287 100__ $$0(orcid)0000-0003-3652-3527$$aCasas, A.M.$$uUniversidad de Zaragoza
000061287 245__ $$aApplication of Anisotropy of Magnetic Susceptibility to large-scale fault kinematics: an evaluation
000061287 260__ $$c2017
000061287 5060_ $$aAccess copy available to the general public$$fUnrestricted
000061287 5203_ $$aMajor discontinuities in the Earth’s crust are expressed by faults that often cut across its whole thickness favoring, for example, the emplacement of magmas of mantelic origin. These long-lived faults are common in intra-plate
environments and show multi-episodic activity that spans for hundred of million years and constitute first-order controls on plate evolution, favoring basin formation and inversion, rotations and the accommodation of deformation in large segments of plates. Since the post-Paleozoic evolution of these large-scale faults has taken place (and can only be observed) at shallow crustal levels, the accurate determination of fault kinematics is hampered
by scarcely developed fault rocks, lack of classical structural indicators and the brittle deformation accompanying fault zones. These drawbacks are also found when thick clayey or evaporite levels, with or without diapiric movements, are the main detachment levels that facilitate large displacements in the upper crust...
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000061287 700__ $$0(orcid)0000-0002-9743-8695$$aRoman-Berdiel, M.T.$$uUniversidad de Zaragoza
000061287 700__ $$aMarcén, M.$$uUniversidad de Zaragoza
000061287 700__ $$aOliva-Urcia, B.
000061287 700__ $$0(orcid)0000-0002-1929-8850$$aSoto, R.
000061287 700__ $$0(orcid)0000-0003-4441-4240$$aGarcia-Lasanta, C.
000061287 700__ $$aCalvin, P.
000061287 700__ $$0(orcid)0000-0003-3197-4177$$aPocovi, A.$$uUniversidad de Zaragoza
000061287 700__ $$0(orcid)0000-0001-6110-1081$$aGil-Imaz, A.$$uUniversidad de Zaragoza
000061287 700__ $$0(orcid)0000-0002-1460-1590$$aPueyo-Anchuela, Ó.$$uUniversidad de Zaragoza
000061287 700__ $$0(orcid)0000-0002-5159-8140$$aIzquierdo-Llavall, E.
000061287 700__ $$aVernet, E.
000061287 700__ $$0(orcid)0000-0002-2408-809X$$aSantolaria, P.
000061287 700__ $$0(orcid)0000-0002-5246-366X$$aOsacar, C.$$uUniversidad de Zaragoza
000061287 700__ $$aSantanach, P.
000061287 700__ $$aCorrado, S.
000061287 700__ $$aInvernizzi, C.
000061287 700__ $$aAldega, L.
000061287 700__ $$aCaricchi, C.
000061287 700__ $$aVillalain, J.J.
000061287 7102_ $$12000$$2428$$aUniversidad de Zaragoza$$bDepartamento de Ciencias de la Tierra$$cGeodinámica Interna
000061287 7102_ $$12000$$2120$$aUniversidad de Zaragoza$$bDepartamento de Ciencias de la Tierra$$cCristalografía y Mineralogía
000061287 7102_ $$12000$$2655$$aUniversidad de Zaragoza$$bDepartamento de Ciencias de la Tierra$$cPaleontología
000061287 773__ $$g19 (2017), 15988$$pGeophys. Res. Abstracts$$tGeophysical Research Abstracts$$x1029-7006
000061287 8564_ $$s36750$$uhttp://zaguan.unizar.es/record/61287/files/texto_completo.pdf$$yVersión publicada
000061287 8564_ $$s114466$$uhttp://zaguan.unizar.es/record/61287/files/texto_completo.jpg?subformat=icon$$xicon$$yVersión publicada
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000061287 951__ $$a2017-10-24-12:03:50
000061287 980__ $$aARTICLE