000127756 001__ 127756
000127756 005__ 20231219145820.0
000127756 0247_ $$2doi$$a10.1007/s00531-022-02265-3
000127756 0248_ $$2sideral$$a130994
000127756 037__ $$aART-2023-130994
000127756 041__ $$aeng
000127756 100__ $$aPeiro, Alba
000127756 245__ $$aRecent activity and paleoseismicity of an intraplate extensional fault: the Calamocha fault (Jiloca graben, central Iberian Chain)
000127756 260__ $$c2023
000127756 5060_ $$aAccess copy available to the general public$$fUnrestricted
000127756 5203_ $$aThe Calamocha fault is an 18-km-long, NNW–SSE striking pure normal fault that moves down the northern sector of the Jiloca graben with respect to the Neogene infill of the Calatayud basin (central Iberian Chain). Its structure and kinematics are characterized by means of detailed geological mapping, morphotectonic analysis and data recording at the outcrop scale. The Calamocha fault represents the inversion of a previous contractional fault zone under the recent tensional stress field (WSW–ENE trending σ3 trajectories). The extensional activity started during the Late Pliocene (ca. 3.8 Ma), accumulating a maximum net slip of 190–230 m (long-term slip rate of 0.05–0.06 mm/a). The palaeoseismological study of three artificial exposures near Calamocha town evidenced recurrent slip during the Late Pleistocene, which proves its active character. Analysis of faulted clastic alluvial units, dated by means of optically stimulated luminescence (OSL), reveals at least eight slip events since 145.9 ± 9.1 ka, the last one being younger than 13.8 ± 0.9 ka. Only a few events represent visible accumulated displacement on the main synthetic rupture surfaces; this allows a rough estimate of the short-term slip rate (during the Late Pleistocene) of about 0.1 mm/a, faster than the long-term rate. The Calamocha fault could potentially produce a characteristic earthquake (in the sense of Schwartz and Coppersmith, J Geophys Res 89:5681–5698, 1984) with moment magnitude Mw ≈ 6.7 ± 0.3 (Mw ≈ 6.9 ± 0.3 in a scenario of activation of the whole Calamocha–Daroca fault zone), average coseismic displacement of 0.5–1.3 m and average recurrence period under 15 ka.
000127756 536__ $$9info:eu-repo/grantAgreement/ES/DGA-FEDER/LMP127-18$$9info:eu-repo/grantAgreement/ES/DGA/E32-20R$$9info:eu-repo/grantAgreement/ES/AEI/PID2019-108705GB-I00
000127756 540__ $$9info:eu-repo/semantics/openAccess$$aby$$uhttp://creativecommons.org/licenses/by/3.0/es/
000127756 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/publishedVersion
000127756 700__ $$0(orcid)0000-0003-1412-5245$$aSimón, José L.$$uUniversidad de Zaragoza
000127756 700__ $$0(orcid)0000-0002-2141-2624$$aMartín-Bello, Leticia
000127756 700__ $$0(orcid)0000-0001-5091-9398$$aArlegui, Luis E.$$uUniversidad de Zaragoza
000127756 700__ $$0(orcid)0000-0003-0900-1440$$aEzquerro, Lope$$uUniversidad de Zaragoza
000127756 700__ $$0(orcid)0000-0002-8929-9429$$aLuzón, Aránzazu$$uUniversidad de Zaragoza
000127756 700__ $$aMedialdea, Alicia
000127756 700__ $$aCorral, Belén
000127756 700__ $$0(orcid)0000-0002-9130-117X$$aLiesa, Carlos L.$$uUniversidad de Zaragoza
000127756 7102_ $$12000$$2655$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Paleontología
000127756 7102_ $$12000$$2428$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Geodinámica Interna
000127756 7102_ $$12000$$2280$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Estratigrafía
000127756 773__ $$g112 (2023), 513-537$$pInt. j. earth sci.$$tInternational Journal of Earth Sciences$$x1437-3254
000127756 8564_ $$s2448356$$uhttps://zaguan.unizar.es/record/127756/files/texto_completo.pdf$$yVersión publicada
000127756 8564_ $$s1802718$$uhttps://zaguan.unizar.es/record/127756/files/texto_completo.jpg?subformat=icon$$xicon$$yVersión publicada
000127756 909CO $$ooai:zaguan.unizar.es:127756$$particulos$$pdriver
000127756 951__ $$a2023-12-19-14:46:37
000127756 980__ $$aARTICLE