Hostname: page-component-cd9895bd7-7cvxr Total loading time: 0 Render date: 2024-12-23T15:45:14.951Z Has data issue: false hasContentIssue false
  • English
  • Français

The Río Grío–Pancrudo Fault Zone (central Iberian Chain, Spain): recent extensional activity revealed by drainage reversal

Published online by Cambridge University Press:  09 September 2021

Alba Peiro Open the ORCID record for Alba Peiro [Opens in a new window]  and
José L. Simón
Alba Peiro*
Affiliation:
Dpto Ciencias de la Tierra, Grupo Geotransfer-IUCA, Universidad de Zaragoza, Pedro Cerbuna 12, 50009Zaragoza, Spain
José L. Simón
Affiliation:
Dpto Ciencias de la Tierra, Grupo Geotransfer-IUCA, Universidad de Zaragoza, Pedro Cerbuna 12, 50009Zaragoza, Spain
*
Author for correspondence: Alba Peiro, Email: [email protected]
Get access Rights & Permissions [Opens in a new window]

Abstract

The NNW–SSE-trending extensional Río Grío–Pancrudo Fault Zone is a large-scale structure that obliquely cuts the Neogene NW–SE Calatayud Basin. Its negative inversion during the Neogene–Quaternary extension gave rise to structural and geomorphological rearrangement of the basin margin. Geological mapping has allowed two right-relayed fault segments to be distinguished, whose recent extensional activity has been mainly characterized using a deformed planation surface (Fundamental Erosion Surface (FES) 3; 3.5 Ma) as a geomorphic marker. Normal slip along the Río Grío–Lanzuela Fault Segment has induced hanging-wall tilting, subsequent drainage reversal at the Güeimil valley after the Pliocene–Pleistocene transition, as well as morphological scarps and surficial ruptures in Pleistocene materials. In this sector, an offset of FES3 indicates a total throw of c. 240 m, resulting in a slip rate of 0.07 mm a–1, while retrodeformation of hanging-wall tilting affecting a younger piedmont surface allows the calculation of a minimum throw in the range of 140–220 m after the Pliocene–Pleistocene transition, with a minimum slip rate of 0.07–0.11 mm a–1. For the late Pleistocene period, vertical displacement of c. 20 m of a sedimentary level dated to 66.6 ± 6.5 ka yields a slip rate approaching 0.30–0.36 mm a–1. At the Cucalón–Pancrudo Fault Segment, the offset of FES3 allows the calculation of a maximum vertical slip of 300 m for the last 3.5 Ma, and hence a net slip rate close to 0.09 mm a–1. Totalling c. 88 km in length, the Río Grío–Pancrudo Fault Zone could be the largest recent macrostructure in the Iberian Chain, probably active, with the corresponding undeniable seismogenic potential.

Keywords

Calatayud Basinrecent faultactive faulttectonic geomorphologyplanation surfacePlio-Quaternaryslip rate
Type
Original Article
Information
Geological Magazine , Volume 159 , Issue 1 , January 2022 , pp. 21 - 36
Copyright
© The Author(s), 2021. Published by Cambridge University Press

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Adrover, R (1975) Principales yacimientos paleomastológicos de la provincia de Teruel y su posición estratigráfica relativa. In Actas I Coloquio Internacional sobre Bioestratigrafía Continental del Neógeno Superior-Cuaternario Inferior (eds Alberdi, MT and Aguirre, E), pp. 31–48. Madrid-Montpellier: Trabajos sobre Neógeno-Cuaternario.Google Scholar
Adrover, R, Feist, M, Hugueney, M, Mein, P and Moissenet, E (1982) L’âge et la mise en relief de la formation detritique culminante de la Sierra Pelarda (Prov. Teruel, Espagne). Comptes rendus de l’Académie des sciences, Paris 295, 231–6.Google Scholar
Allmendinger, RW, Cardozo, NC and Fisher, D (2012) Structural Geology Algorithms: Vectors & Tensors. Cambridge: Cambridge University Press, 289 p.Google Scholar
Álvaro, M, Capote, R and Vegas, R (1979) Un modelo de evolución geotectónica para la Cadena Celtibérica. Acta Geologica Hispánica 14, 172–7.Google Scholar
Anadón, P, Alcalá, L, Alonso-Zarza, AM, Calvo, JP, Ortí, F, Rosell, L and Sanz-Rubio, E (2004) Cuencas de la Cordillera Ibérica. In Geología de España (ed Vera, JA), pp. 562–69. Madrid: Sociedad Geológica de España-Instituto Geológico y Minero de España.Google Scholar
Aragonés, E, Hernández, A, Aguilar, MJ, Ramírez, J, García-Alcalde, GL and Arbizu, M (1981) Mapa Geológico de España 1: 50.000, hoja no. 409 (Calatayud). Madrid: Instituto Geológico y Minero de España.Google Scholar
Arlegui, LE, Simón, JL, Lisle, RJ and Orife, T (2005) Late Pliocene–Pleistocene stress field in the Teruel and Jiloca grabens (eastern Spain): contribution of a new method of stress inversion. Journal of Structural Geology 27, 693–705.CrossRefGoogle Scholar
Bentham, P, Collier, RE, Gawthorpe, RL, Leeder, R and Stark, C (1991) Tectono-sedimentary development of an extensional basin: the Neogene Megara Basin, Greece. Journal of the Geological Society 148, 923–34.CrossRefGoogle Scholar
Biasi, GP and Wesnousky, SG (2016) Steps and gaps in ground ruptures: empirical bounds on rupture propagation. Bulletin of the Seismological Society of America 106, 1110–24.CrossRefGoogle Scholar
Bonow, JM, Lidmar-Bergström, K and Japsen, P (2006) Palaeosurfaces in central West Greenland as reference for identification of tectonic movements and estimation of erosion. Global and Planetary Change 50, 161–83.CrossRefGoogle Scholar
Burbank, DW and Anderson, RS (2012) Tectonic Geomorphology. Oxford: Wiley-Blackwell, 454 p.Google Scholar
Calvín-Ballester, P and Casas, A (2014) Folded Variscan thrusts in the Herrera unit of the Iberian Range (NE Spain). In Deformation Structures and Processes within the Continental Crust (eds S Llana-Fúnez, A Marcos and F Bastida), pp. 39–52. Geological Society of London, Special Publication no. 394.CrossRefGoogle Scholar
Campos, S, Aurell, M and Casas, A (1996) Origen de las brechas de la base del Jurásico en Morata de Jalón. Geogaceta 20, 887–9.Google Scholar
Capote, R, Muñoz, JA, Simón, JL, Liesa, CL and Arlegui, LE (2002) Alpine tectonics I: The Alpine system north of the Betic Cordillera. In Geology of Spain (eds Gibbons, W and Moreno, T), pp. 367–400. Geological Society of London.CrossRefGoogle Scholar
Cardozo, N and Allmendinger, RW (2013) Spherical projections with OSXStereonet. Computers & Geosciences 51, 193–205.CrossRefGoogle Scholar
Casas, A, Aurell, M, Revuelto, C, Calvín, P, Simón, JL, Pueyo, Ó, Pocoví, A and Marcén, M (2017) El embalse de Mularroya (Zaragoza): problemas geológicos de una obra en estado avanzado de construcción. Revista de la Sociedad Geológica de España 30, 51–64.Google Scholar
Casas, A, Marcén, M, Calvín, P, Gil, A, Román-Berdiel, T and Pocoví, A (2016) Deformación varisca, tardivarisca y alpina en la Rama Aragonesa de la Cordillera Ibérica: propuesta para diferenciación y denominación de estructuras. Geo-Temas 16, 495–8.Google Scholar
Colomer, M and Santanach, P (1988) Estructura y evolución del borde sur-occidental de la Fosa de Calatayud-Daroca. Geogaceta 4, 29–31.Google Scholar
Cortés-Gracia, AL and Casas-Sáinz, A (1996) Deformación alpina de zócalo y cobertera en el borde norte de la Cordillera Ibérica (Cubeta de Azuara-Sierra de Herrera). Revista de la Sociedad Geológica de España 9, 51–66.Google Scholar
Dade, WB and Verdeyen, ME (2007) Tectonic and climatic controls of alluvial-fan size and source-catchment relief. Journal of the Geological Society, 164, 353–8.CrossRefGoogle Scholar
de Vicente, G, Vegas, R, Muñoz-Martín, A, Wees, JDVan, Casas-Sáinz, A, Sopeña, A, Sánchez-Moya, Y, Arche, A, López-Gómez, J, Olaiz, A and Fernández-Lozano, J (2009) Oblique strain partitioning and transpression on an inverted rift: The Castilian Branch of the Iberian Chain. Tectonophysics 470, 224–42.CrossRefGoogle Scholar
del Olmo, P, Hernández, A, Aragonés, E, Gutiérrez, M, Puigdefábregas, C, Giner, J, Aguilar, MJ, Leal, MC, Gutiérrez, JC, Gil, M, Adrover, R, Portero, JM and Gabaldón, V (1983a) Mapa Geológico de España 1: 50.000, hoja no. 437 (Ateca). Madrid: Instituto Geológico y Minero de España.Google Scholar
del Olmo, P, Portero, JM, Villena, J, Pardo, G, Gutiérrez, M, Puigdefábregas, C, Giner, J, Aguilar, MJ, Leal, MC, Goy, A, Comas, MJ and Gabaldón, V (1983b) Mapa Geológico de España 1: 50.000, hoja no. 490 (Odón). Madrid: Instituto Geológico y Minero de España.Google Scholar
Ezquerro, L (2017) El sector norte de la cuenca neógena de Teruel: tectónica, clima y sedimentación. Ph.D. thesis, Universidad de Zaragoza. Published thesis.Google Scholar
Ezquerro, L, Lafuente, P, Pesquero, MD, Alcalá, L, Arlegui, LE, Liesa, CL, Luque, L, Rodríguez-Pascua, MA and Simón, JL (2012) Una cubeta endorreica residual Plio-Pleistocena en la zona de relevo entre las fallas de Concud y Teruel: implicaciones paleogeográficas. Revista de la Sociedad Geológica de España 25, 157–75.Google Scholar
Ezquerro, L, Luzón, A, Liesa, CL and Simón, JL (2019) Alluvial sedimentation and tectono-stratigraphic evolution in a narrow extensional zigzag basin margin (northern Teruel Basin, Spain). Journal of Palaeogeography 8, 1–25.CrossRefGoogle Scholar
Ezquerro, L, Simón, JL, Luzón, A and Liesa, CL (2020) Segmentation and increasing activity in the Neogene-Quaternary Teruel Basin rift (Spain) revealed by morphotectonic approach. Journal of Structural Geology 135, published online 26 March 2020. doi: 10.1016/j.jsg.2020.104043 CrossRefGoogle Scholar
Gabaldón, V, Lendínez, A, Ferreiro, E, Ruiz, V, López de Alda, F, Valverde, M, Lago San José, M, Meléndez, A, Pardo, G, Ardevol, L, Villena, J, González, A, Hernández, A, Álvaro, M, Leal, MC, Aguilar Tomás, M, Gómez, JJ and Carls, P (1991) Mapa Geológico de España 1: 200.000, hoja no. 40 (Daroca). Madrid: Instituto Geológico y Minero de España.Google Scholar
Gabaldón, V, Lendínez, A, Ruiz, V, Carls, P, Alvaro, M, Guitérrez, M, Hernández, A, Gómez, JJ, Meléndez, A, Perez, A, Pardo, G, Villena, J, Aguilar, M, Leal, MC, Comas, MJ, Goy, A, Lago, M and Conte, JC (1989a) Mapa Geológico de España 1: 50.000, hoja no. 466 (Moyuela). Madrid: Instituto Geológico y Minero de España.Google Scholar
Gabaldón, V, Lendínez, A, Ruiz, V, Carls, P, Alvaro, M, Guitérrez, M, Soriano, MA, Hernández, A, Gómez, JJ, Meléndez, A, Aurell, M, Pérez, A, Pardo, G, Villena, J, Aguilar, M, Leal, MC, Comas, MJ, Goy, A, Lago, M and Conte, JC (1989b) Mapa Geológico de España 1: 50.000, hoja no. 439 (Azuara). Madrid: Instituto Geológico y Minero de España.Google Scholar
Goldsworthy, M and Jackson, J (2000) Active normal fault evolution in Greece revealed by geomorphology and drainage patterns. Journal of the Geological Society 157, 967–81.CrossRefGoogle Scholar
Gracia, FJ, Gutiérrez, M and Leránoz, B (1988) Las superficies de erosión neógenas en el sector central de la Cordillera Ibérica. Revista de la Sociedad Geológica de España 1, 135–42.Google Scholar
Gracia, J (1992) Tectónica pliocena de la Fosa de Daroca (prov. de Zaragoza). Geogaceta 11, 127–9.Google Scholar
Guimerà, J (1988) Estudi estructural de l’enllaç entre la Serralada Iberica y la Serralada Costanera Catalana. Ph.D. thesis, Universitat de Barcelona. Published thesis.Google Scholar
Gutiérrez, F, Gracia, FJ and Gutiérrez, M (1996) Consideraciones sobre el final del relleno endorreico de las fosas de Calatayud y Teruel y su paso al exorreismo: implicaciones morfoestratigráficas y estructurales. In IV Reunión de Geomorfología (eds Grandal, A and Pagés, J), pp. 23–43. O Castro, A Coruña: Sociedad Española de Geomorfología.Google Scholar
Gutiérrez, F, Gutiérrez, M, Gracia, FJ, McCalpin, JP, Lucha, P and Guerrero, J (2008) Plio-Quaternary extensional seismotectonics and drainage network development in the central sector of the Iberian Chain (NE Spain). Geomorphology 102, 21–42.CrossRefGoogle Scholar
Gutiérrez, F, Lucha, P and Jordá, L (2013) The Río Grío depression (Iberian Chain, NE Spain). Neotectonic graben vs. Fluvial valley. Cuaternario y Geomorfología 27, 5–32.Google Scholar
Gutiérrez, F, Moreno, D, López, GI, Jiménez, F, del Val, M, Alonso, MJ, Martínez-Pillado, V, Guzmán, O, Martínez, D and Carbonel, D (2020) Revisiting the slip rate of Quaternary faults in the Iberian Chain, NE Spain. Geomorphic and seismic-hazard implications. Geomorphology, 363, 107233.CrossRefGoogle Scholar
Haworth, RJ and Ollier, CD (1992) Continental rifting and drainage reversal: the Clarence River of eastern Australia. Earth Surface Processes and Landforms 17, 387–97.CrossRefGoogle Scholar
Hernández, A, Olivé, A, Moissenet, E, Pardo, G, Villena, J, Portero, JM, Gutiérrez, M, Puigdefábregas, C, Giner, J, Aguilar, MJ, Leal, MC, Gutiérrez, JC, Gil, MD, Adrover, R and Gabaldón, V (1983) Mapa Geológico de España 1: 50.000, hoja no. 491 (Calamocha). Madrid: Instituto Geológico y Minero de España.Google Scholar
Hernández, A, Ramírez, JI, Navarro, JJ, Cortes, AL, Rodríguez, R, Babiano, F, Gómez, D, Ramírez, J, Cuenca, G, Pozo, M and Casas, J (2005) Mapa Geológico de España 1: 50.000, hoja no. 411 (Longares). Madrid: Instituto Geológico y Minero de España.Google Scholar
Herraiz, M, De Vicente, G, Lindo-Ñaupari, R, Giner, J, Simón, JL, González-Casado, JM, Vadillo, O, Rodríguez-Pascua, MA, Cicuéndez, JL, Casas, A, Cabañas, L, Rincón, P, Cortés, AL, Ramírez, M and Lucini, M (2000) The recent (upper Miocene to Quaternary) and present tectonic stress distributions in the Iberian Peninsula. Tectonics 19, 762–86.CrossRefGoogle Scholar
Jackson, J, Norris, R and Youngson, J (1996) The structural evolution of active fault and fold systems in central Otago, New Zealand: evidence revealed by drainage patterns. Journal of Structural Geology 18, 217–34.CrossRefGoogle Scholar
Jackson, JA and McKenzie, D (1983) The geometrical evolution of normal fault systems. Journal of Structural Geology 5, 471–82.CrossRefGoogle Scholar
Jackson, JA, White, NJ, Garfunkel, Z and Anderson, H (1988) Relations between normal fault geometry, tilting and vertical motions in extensional terrains: an example from the southern Gulf of Suez. Journal of Structural Geology 10, 155–70.CrossRefGoogle Scholar
Julivert, M (1954) Observaciones sobre la tectónica de la Depresión de Calatayud. Sabadell: Museo de Sabadell, 17 p.Google Scholar
Keller, EA (1986) Investigation of active tectonics: use of surficial earth processes. In Active Tectonics: Impact on Society (ed Wallace, RR), pp. 136–147. Washington DC: National Academic Press.Google Scholar
Lafuente, P, Arlegui, LE, Liesa, CL, Pueyo, O and Simón, JL (2014) Spatial and temporal variation of paleoseismic activity at an intraplate, historically quiescent structure: the Concud fault (Iberian Chain, Spain). Tectonophysics 632, 167–87.CrossRefGoogle Scholar
Leeder, MR and Jackson, JA (1993) The interaction between normal faulting and drainage in active extensional basins, with examples from the western United States and central Greece. Basin Research 5, 79–102.CrossRefGoogle Scholar
Leeder, MR, Seger, MJ and Stark, CP (1991) Sedimentation and tectonic geomorphology adjacent to major active and inactive normal faults, southern Greece. Journal of the Geological Society 148, 331–43.CrossRefGoogle Scholar
Liesa, CL, Simón, JL, Ezquerro, L, Arlegui, LE and Luzón, A (2019) Stress evolution and structural inheritance controlling an intracontinental extensional basin: the central-northern sector of the Neogene Teruel Basin. Journal of Structural Geology 118, 362–76.CrossRefGoogle Scholar
Maillard, A and Mauffret, A (1999) Crustal structure and riftogenesis of the Valencia Trough (north-western Mediterranean Sea). Basin Research, 11, 357–79.CrossRefGoogle Scholar
Marcén, M (2020) Fábricas Magnéticas aplicadas al estudio de Zonas de Falla: Ejemplos de la Península Ibérica. Ph.D. thesis, Universidad de Zaragoza. Published thesis.Google Scholar
Marcén, M and Román-Berdiel, MT (2015) Geometría y cinemática de la zona de falla de Río Grío: evidencias de transpresión alpina en la Cadena Ibérica. Geogaceta 58, 180–3.Google Scholar
Martín, M, Canerot, J, Linares-Rivas, A, Grambast, L, Quintero, I, Mansilla, H, De las Heras, A, Fernández, MC, Leyva, F and Martínez, JU (1977) Mapa Geológico de España 1: 50.000, hoja no. 492 (Segura de los Baños). Madrid: Instituto Geológico y Minero de España.Google Scholar
Martín-Bello, L, Arlegui, LE, Ezquerro, L, Liesa, CL and Simón, JL (2014) La falla de Calamocha (fosa del Jiloca, Cordillera Ibérica): estructura y actividad pleistocena. In Una aproximación multidisciplinary al studio de las fallas activas, los terremotos y el riesgo sísmico (eds Álvarez-Gómez, A and Martín-González, F), pp. 55–58. Lorca, Murcia, 22–24 October 2014. 2ª Reunión Ibérica sobre Fallas Activas y Paleosismología.Google Scholar
Masana, E (1995) L’activitat neotectònica a les cadenes Costaneres Catalanes. Ph.D. thesis, Universitat de Barcelona. Published thesis.Google Scholar
Masana, E, Villamarín, JA and Santanach, P (2001) Paleoseismic results from multiple trenching analysis along a silent fault: the El Camp fault (Tarragona, northeastern Iberian Peninsula). Acta Geologica Hispánica 36, 329–54.Google Scholar
Mateu, J (1982) El Norte del País Valenciano. Geomorfología litoral y prelitoral. Ph.D. thesis, Universitat de Valencia. Published thesis.Google Scholar
Matmon, A, Enzel, Y, Zilberman, E and Heimann, A (1999) Late Pliocene and Pleistocene reversal of drainage systems in northern Israel: tectonic implications. Geomorphology 28, 43–59.CrossRefGoogle Scholar
McCalpin, JP (1996) Paleoseismology. San Diego: Academic Press, 588 p.Google Scholar
Moissenet, É (1980) Relief et déformations récentes: trois transversales dans les fossés internes des chaînes ibériques orientales. Revue géographique des Pyrénées et du Sud-Ouest, Sud-Ouest Européen 51, 315–44.CrossRefGoogle Scholar
Olivé, A, del Olmo, P, Portero, JM, Carls, P, Sdzuy, K, Collande, CV, Kolb, S, Teyssen, T, Gutiérrez, M, Puigdefábregas, C, Giner, J, Aguilar, MJ, Leal, MC, Goy, A, Comas, MJ, Adrover, R and Gabaldón, V (1983) Mapa Geológico de España 1: 50.000, hoja no. 438 (Paniza). Madrid: Instituto Geológico y Minero de España.Google Scholar
Olivé, A, Hernández, A, Moissenet, E, Pardo, G, Villena, J, Gutiérrez, M, Puigdefábregas, C, Giner, J, Aguilar, MJ, Leal, MC, Goy, A, Comas, MJ, Adrover, R, Portero, JM and Gabaldón, V (2002) Mapa Geológico de España 1: 50.000, hoja no. 516 (Monreal del Campo). Madrid: Instituto Geológico y Minero de España.Google Scholar
Ollier, C (1981) Tectonics and Landforms. London: Longman, 324 pp.Google Scholar
Pailhé, P (1984) La Chaîne Ibérique Orientale. Étude géomorphologique. Ph.D. thesis, Université de Bordeaux. Published thesis.Google Scholar
Peña, JL, Gutiérrez, M, Ibáñez, MJ, Lozano, MV, Rodríguez, J, Sánchez-Fabre, M, Simón, JL, Soriano, MA and Yetano, LM (1984) Geomorfología de la provincia de Teruel. Teruel: Instituto de Estudios Turolenses, 149 p.Google Scholar
Perea, H, Masana, E and Santanach, P (2006) A pragmatic approach to seismic parameters in a region with low seismicity: the case of Eastern Iberia. Natural Hazards 39, 451–77.CrossRefGoogle Scholar
Pérez, A, Pardo, G, Villena, J and González, A (1983) Estratigrafía y sedimentología del Paléogeno de la cubeta de Montalbán, prov. de Teruel, España. Boletín de la Real Sociedad Española de Historia Natural, Sección Geológica 81, 197–223.Google Scholar
Pérez, A and Simón, JL (1993) Cambios en el trazado de la red fluvial producidos por la tectónica cuaternaria en el sistema de fosas del Maestrat. El Cuaternario de España y Portugal, ITGE-AEQUA, Madrid 2, 707–15.Google Scholar
Roberts, GP, Michetti, AM, Cowie, P, Morewood, NC and Papanikolaou, I (2002) Fault slip-rate variations during crustal-scale strain localisation, central Italy. Geophysical Research Letters 29, 9-1.CrossRefGoogle Scholar
Roca, E and Guimerá, J (1992) The Neogene structure of the eastern Iberian margin: structural constraints on the crustal evolution of the Valencia trough (western Mediterranean). Tectonophysics 203, 203–18.CrossRefGoogle Scholar
Rubio, JC (2004) Estudio hidrogeológico e histórico arqueológico de los humedales del alto Jiloca. Zaragoza: Consejo de Protección de la Naturaleza de Aragón, 216 p.Google Scholar
Rubio, JC and Simón, JL (2007) Tectonic subsidence vs. erosional lowering in a controversial intramontane depression: the Jiloca basin (Iberian Chain, Spain), Geological Magazine 144, 1–15.CrossRefGoogle Scholar
Sanz-Rubio, E (1999) Análisis de los sistemas deposicionales carbonáticos y evaporíticos del Neógeno de la Cuenca de Calatayud (provincia de Zaragoza). Ph.D. thesis, Universidad Complutense de Madrid. Published thesis.Google Scholar
Sanz-Rubio, E, Sánchez-Moral, S, Cañaveras, JC, Abdul-Aziz, H, Calvo, JP, Cuezva, S, Mazo, AV, Rouchy, JM, Sesé, C and Van Darn, J (2003) Síntesis de la cronoestratigrafía y evolución sedimentaria de los sistemas lacustres evaporíticos y carbonatados neógenos de la cuenca de Calatayud-Montalbán. Estudios Geológicos 59, 83–105.CrossRefGoogle Scholar
Scotti, VN, Molin, P, Faccenna, C, Soligo, M and Casas-Sainz, A (2014) The influence of surface and tectonic processes on landscape evolution of the Iberian Chain (Spain): quantitative geomorphological analysis and geochronology. Geomorphology 206, 37–57.CrossRefGoogle Scholar
Simón, JL (1982) Compresión y distensión alpinas en la Cadena Ibérica Oriental. Ph.D. thesis, Universidad de Zaragoza. Published thesis.Google Scholar
Simón, JL (1989) Late Cenozoic stress field and fracturing in the Iberian Chain and Ebro Basin (Spain). Journal of Structural Geology 11, 285–94.CrossRefGoogle Scholar
Simón, JL, Arlegui, LE, Ezquerro, L, Lafuente, P, Liesa, CL and Luzón, A (2016) Enhanced palaeoseismic succession at the Concud Fault (Iberian Chain, Spain): new insights for seismic hazard assessment. Natural Hazards 80, 1967–93.CrossRefGoogle Scholar
Simón, JL, Arlegui, LE, Ezquerro, L, Lafuente, P, Liesa, CL and Luzón, A (2017) Assessing interaction of active extensional faults from structural and paleoseismological analysis: The Teruel and Concud faults (eastern Spain). Journal of Structural Geology 103, 100–19.CrossRefGoogle Scholar
Simón, JL, Arlegui, L, Lafuente, P and Liesa, CL (2012) Active extensional faults in the central-eastern Iberian Chain, Spain. Journal of Iberian Geology 38, 127–44.CrossRefGoogle Scholar
Simón, JL, Ezquerro, L, Arlegui, LE, Liesa, CL, Luzón, A, Medialdea, A, García, A and Zarazaga, D (2019) Role of transverse structures in paleoseismicity and drainage rearrangement in rift systems: the case of the Valdecebro fault zone (Teruel graben, eastern Spain). International Journal of Earth Sciences 108, 1429–49.CrossRefGoogle Scholar
Simón, JL, Pérez-Cueva, AJ and Calvo-Cases, A (2013) Tectonic beheading of fluvial valleys in the Maestrat grabens (eastern Spain): insights into slip rates of Pleistocene extensional faults. Tectonophysics 593, 73–84.CrossRefGoogle Scholar
Simón-Porcar, G, Simón, JL and Liesa, CL (2019) La cuenca neógena extensional de El Pobo (Teruel, Cordillera Ibérica): sedimentología, estructura y relación con la evolución del relieve. Revista de la Sociedad Geológica de España 32, 17–42.Google Scholar
Sinusía, C, Pueyo, EL, Azanza, B and Pocoví, A (2004) Datación magnetoestratigráfica del yacimiento paleontológico de La Puebla de Valverde (Teruel). Geo-Temas 6, 339–42.Google Scholar
Tena, S and Casas, A (1996) Estructura y cinemática de la falla de Alpeñés (Cordillera Ibérica). Geogaceta 20, 789–91.Google Scholar
Vacherat, A, Bonnet, S and Mouthereau, F (2018) Drainage reorganization and divide migration induced by the excavation of the Ebro basin (NE Spain). Earth Surface Dynamics 6, 369–387.CrossRefGoogle Scholar
Vegas, R, Fontboté, JM and Banda, E (1979) Widespread Neogene rifting superimposed on alpine regions of the Iberian Peninsula. Proceedings of the Symposium on Evolution and Tectonics of the Western Mediterranean and Surrounding Areas, EGS, Vienna. Madrid: Instituto Geográfico Nacional, Special Publication no. 201, 109–128.Google Scholar
Wagner, T, Fritz, H, Stüwe, K, Nestroy, O, Rodnight, H, Hellstrom, J and Benischke, R (2011) Correlations of cave levels, stream terraces and planation surfaces along the River Mur: Timing of landscape evolution along the eastern margin of the Alps. Geomorphology 134, 62–78.CrossRefGoogle ScholarPubMed
Wells, DL and Coppersmith, KJ (1994) New empirical relationships among magnitude, rupture length, rupture width, rupture area and surface displacement. Bulletin of the Seismological Society of America 84, 974–1002.Google Scholar
Supplementary material: File

Peiro and Simón supplementary material

Peiro and Simón supplementary material

Download Peiro and Simón supplementary material(File)
File 97.3 KB