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Discussion of ‘Tectonic subsidence v. erosional lowering in a controversial intramontane depression: the Jiloca basin (Iberian Chain, Spain)’

Published online by Cambridge University Press:  29 April 2008

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F. J. Gracia, F. Gutiérrez & M. Gutiérrez comment: In a recent paper, Rubio & Simón (2007) propose that the origin of the Jiloca Depression (Iberian Range, NE Spain) is primarily due to extensional neotectonics and estimate a Plio-Quaternary vertical offset of 350–400 m on the basin-bounding master fault. However, these authors omit crucial evidence presented in previous papers that contradict their model and derive interpretations from ambiguous or erroneous data. This discussion presents the main objections to their model and supports the mixed erosional (karstic) and tectonic origin proposed in previous research articles.

Keywords

poljeneotectonicsIberian RangeSpain
Type
Discussion
Information
Geological Magazine , Volume 145 , Issue 4 , July 2008 , pp. 591 - 597
Copyright
Copyright © Cambridge University Press 2008

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References

Arlegui, L. E., Simón, J. L., Lisle, R. J. & Orife, T. 2006. Analysis of non-striated faults in a recent extensional setting: the Plio-Pleistocene Concud fault (Jiloca graben, eastern Spain). Journal of Structural Geology 28, 1019–27.CrossRefGoogle Scholar
Capote, R., Muñoz, J. A., Simón, J. L., Liesa, C. L. & Arlegui, L. E. 2002. Alpine tectonics I: the Alpine system north of the Betic Cordillera. In The Geology of Spain (eds Gibbons, W. & Moreno, T.), pp. 367–400. London: The Geological Society of London.CrossRefGoogle Scholar
Casas, A. M. & Cortés, A. L. 2002. Cenozoic landscape development within the Central Iberian Chain, Spain. Geomorphology 44, 19–46.Google Scholar
Cortés, A. L. & Casas, A. M. 2000. Tiene el sistema de fosas de Teruel origen extensional? Revista de la Sociedad Geológica de España 13, 445–70.Google Scholar
Ford, D. & Williams, P. 2007. Karst Hydrogeology and Geomorphology. Chichester: John Wiley & Sons, 562p.CrossRefGoogle Scholar
Gams, I. 2005. Tectonics impact on poljes and minor basins (case studies of Dinaric karst). Acta Carstologica 34, 25–41.Google Scholar
Gracia, F. J., Gutiérrez, F. & Gutiérrez, M. 2002. Origin and evolution of the Gallocanta polje (Iberian Range, NE Spain). Zeitschrift für Geomorphologie 46, 245–62.CrossRefGoogle Scholar
Gracia, F. J., Gutiérrez, F. & Gutiérrez, M. 2003. The Jiloca karst polje-tectonic graben (Iberian Range, NE Spain). Geomorphology 52, 215–31.CrossRefGoogle Scholar
Gutiérrez, F. 1998. Efectos de la subsidencia por disolución de evaporitas en sistemas aluviales. El caso del valle del Alfambra en la Fosa de Teruel (Cordillera Ibérica). In XXXII Curso de Geología Práctica (ed. Meléndez, A.), pp. 119–46. Teruel: Universidad de Verano de Teruel.Google Scholar
Gutiérrez, F., Gutiérrez, M & Gracia, F. J. 2005. Karst, neotectonics and periglacial features in the Iberian Range. In Field Trip Guides of the Sixth International Conference on Geomorphology (eds Desir, G., Gutiérrez, F. & Gutiérrez, M.), pp. 341–400. Zaragoza: Sociedad Española de Geomorfología.Google Scholar
Gutiérrez, F., Gutiérrez, M., Gracia, F. J., Lucha, P. & Guerrero, J. 2007. Plio-Quaternary extensional seismotectonics and drainage network development in the central sector of the Iberian Chain (NE Spain). Geomorphology (in press).CrossRefGoogle Scholar
Gutiérrez, M. & Gracia, F. J. 1997. Environmental interpretation and evolution of the Tertiary erosion surfaces in the Iberian Range (Spain). In Palaeosurfaces: Recognition, Reconstruction and Palaeoenvironmental Interpretation (ed. M. Widdowson), pp. 147–58. Geological Society of London Special Puublication no. 120.Google Scholar
Leeder, M. R. & Gawthorpe, R. L. 1987. Sedimentary models for extensional tilt-block/half-graben basins. In Continental Extensional Tectonics (eds Coward, M. P., Dewey, J. F. & Hancock, P. L.), pp. 139–52. London: Geological Society Special Publication no. 28.Google Scholar
Mijatovic, B. F. 1984. Karst poljes in Dinarides. In Hydrogeology of the Dinaric Karst (ed. Mijatovic, B. F.), pp. 87–109. Hannover: International Association of Hydrogeologists.Google Scholar
Moissenet, E. 1984. Observations préliminaires sur les piémonts intérieurs des Monts ibériques dans la région de Teruel. Montagnes et piémonts. Revue de Géographie des Pyrénées et Sud-Ouest 1984, 187–208.Google Scholar
Moissenet, E. 1985. Les dépressions tarditectoniques des Chaînes Ibériques méridionales: distension, diapirisme et dépôts associés. Compte Rendus de l'Academie du Sciences de Paris 11, 523–8.Google Scholar
Peña Monné, J. L., Gutiérrez Elorza, M., Ibáñez Marcellán, M., Lozano Tena, M. Y., Rodríguez Vidal, J., Sánchez Fabre, M., Simón Gómez, J. L., Soriano Jiménez, M. A. & Yetano Ruiz, L. M. 1984. Geomorfología de la Provincia de Teruel. Teruel: Instituto de Estudios Turolenses, 149p.Google Scholar
Ramírez, J. L., Olivé, A. & Moissenet, E. 1981. Memoria y mapa geológico de España, E. 1:50000. Hoja no. 541, Santa Eulalia. Madrid: Instituto Geológico y Minero de España, 71p.Google Scholar
Rubio, J. C. & Simón, J. L. 2007. Tectonic subsidence v. erosional lowering in a controversial intramontane depression: the Jiloca basin (Iberian Chain, Spain). Geological Magazine 144, 127–41.CrossRefGoogle Scholar
Rubio, J. C., Simón, J. L. & Soriano, M. A. 2007. Interacting tectonics, hydrogeology and karst processes in an intramontane basin: the Jiloca graben (NE Spain). Hidrogeology Journal 15, 1565–76.CrossRefGoogle Scholar
Simón, J. L. 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, J. L. & Soriano, A. 1993. La falla de Concud (Teruel): actividad cuaternaria y régimen de esfuerzos asociado. In El Cuaternario de España y Portugal (eds Aleixane, T. & Pérezdr González, A.), pp. 729–37. Madrid: Instituto Tecnológico GeoMinero de España.Google Scholar
Simón, J. L., Lafuente, P., Arlegui, L. I., Liesa, C. L. & Soriano, M. A. 2005. Caracterización paleosísmica de la falla de Concud (fosa del Jiloca, Teruel). Geogaceta 38, 63–6.Google Scholar
Gracia, F. J. Departamento de Ciencias de la Tierra, Facultad de Ciencias del Mar y Ambientales, Universidad de Cádiz, 11510 Puerto Real, Spain; email: Google Scholar
Gutiérrez, F. & Gutiérrez, M. Edificio Geológicas, Universidad de Zaragoza, C/. Pedro Cerbuna 12, 50009 Zaragoza, SpainGoogle Scholar
Rubio, J. C. & Simón, J. L. Departamento de Geología, Universidad de Zaragoza, Pedro Cerbuna 12, 50009 Zaragoza, Spain; email: Google Scholar