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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/4012
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dc.contributor.authorallTent-Manclús, J. E.; Departamento de Ciencias de la Tierra y del Medio Ambiente, Universidad de Alicante, Apto. 99, 03080 San Vicente del Raspeig, Alicante, Spainen
dc.contributor.authorallSoria, J. M.; Departamento de Ciencias de la Tierra y del Medio Ambiente, Universidad de Alicante, Apto. 99, 03080 San Vicente del Raspeig, Alicante, Spainen
dc.contributor.authorallEstévez, A.; Departamento de Ciencias de la Tierra y del Medio Ambiente, Universidad de Alicante, Apto. 99, 03080 San Vicente del Raspeig, Alicante, Spainen
dc.contributor.authorallLancis, C.; Departamento de Ciencias de la Tierra y del Medio Ambiente, Universidad de Alicante, Apto. 99, 03080 San Vicente del Raspeig, Alicante, Spainen
dc.contributor.authorallCaracuel, J. E.; Departamento de Ciencias de la Tierra y del Medio Ambiente, Universidad de Alicante, Apto. 99, 03080 San Vicente del Raspeig, Alicante, Spainen
dc.contributor.authorallDinarès-Turell, J.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.authorallYébenes, A.; Departamento de Ciencias de la Tierra y del Medio Ambiente, Universidad de Alicante, Apto. 99, 03080 San Vicente del Raspeig, Alicante, Spainen
dc.date.accessioned2008-08-27T13:23:00Zen
dc.date.available2008-08-27T13:23:00Zen
dc.date.issued2008-07en
dc.identifier.urihttp://hdl.handle.net/2122/4012en
dc.description.abstractThe Neogene Fortuna and Bajo Segura basins are located on the northeastern end of the Trans-Alborán Shear Zone (TASZ), on the eastern Betic cordillera. The stratigraphic study of the infilling of these basins has shown two major sedimentary discontinuities. The first one, represented by an erosive surface separating open marine marls from an overlying coastal conglomeratic unit, is linked to the onset of the activity along the TASZ, which in this area indicates the beginning of the Abanilla Thrust emplacement. In the Fortuna Basin, the Tortonian salinity crisis, registered over this older first discontinuity, was therefore related to tectonic processes of the eastern portion of the cordillera and consequently would not have an expression in the western basins. The age of the Tortonian Salinity Crisis has been established with nannofossil biostratigraphy as Latest Tortonian at a somewhat lower stratigraphic position than previously recognized. The second sedimentary discontinuity was developed in relation with the known Mediterranean-wide Messinian salinity crisis.en
dc.language.isoEnglishen
dc.publisher.nameElsevieren
dc.relation.ispartofComptes Rendus Geoscienceen
dc.relation.ispartofseries7 / 340 (2008)en
dc.subjectBetic Cordilleraen
dc.subjectTortonian Salinity Crisisen
dc.subjectMessinian Salinity Crisisen
dc.subjectTrans-Alboran Shear Zoneen
dc.subjectFortuna Basinen
dc.subjectSpainen
dc.titleThe Tortonian salinity crisis in the Fortuna Basin (southeastern Spain): Stratigraphic record, tectonic scenario and chronostratigraphyen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber474-481en
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.10. Stratigraphyen
dc.subject.INGV04. Solid Earth::04.05. Geomagnetism::04.05.06. Paleomagnetismen
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonicsen
dc.identifier.doi10.1016/j.crte.2008.05.003en
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Soria, Architecture and sedimentary facies evolution in a delta stack controlled by fault growth (Betic Cordillera, southern Spain, Late Tortonian), Sediment. Geol. 185 (2006) 79–92. [10] F. Guerrera, A. Martín-Algarra, V. Perrone, Late Oligocene- Miocene syn-/-late-orogenic successions in the western and central Mediterranean Chains from the Betic Cordillera to the southern Apennines, Terra Nova 5 (1993) 525–544. [11] R. Jonk, C. Biermann, Deformation in Neogene sediments of the Sorbas and Vera Basins (SE Spain): constrains on simple-shear deformation and rigid body rotation along major strike-slip faults, J. Struct. Geol. 24 (2002) 963–977. [12] W. Krijgsman, M. Garcés, J. Agustí, I. Raffi, C. Taberner, W.J. Zachariasse, The ‘Tortonian salinity crisis’ of the eastern Betics (Spain), Earth Planet, Sci. Lett. 181 (2000) 497–511. [13] P. Lukowski, P., Évolution tectono-sédimentaire du bassin néogène de Fortuna (Cordillères bétiques orientales, Espagne), unpublished doctoral dissertation, Paris-Sud, Orsay, 1987. [14] P. Lukowski, A. Poisson, Le bassin de Fortuna, Doc. et Trav, IGAL 12–13 (1990) 303–311. [15] J.J. Martínez-Díaz, Stress field variation related to fault interaction in a reverse oblique-slip fault: the Alhama de Murcia fault, Betic Cordillera, Spain, Tectonophysics 356 (2002) 291–305. [16] A. Mauffret, D. Frizon de Lamotte, S. Lallemant, C. Gorini, A. Maillard, East–West opening of the Algerian Basin (western Mediterranean), Terra Nova 16 (2004) 257–264. [17] A. Michard, A. Chalouan, H. Feinberg, B. Goffé, R. Montigny, How does the Alpine belt end between Spain and Morocco? Bull. Soc. Geol. France 173 (2002) 3–15. [18] C. Montenat, Les bassins néogènes du levant d’Alicante et de Murcia (Cordillères bétiques orientales – Espagne). Stratigraphie, paléogéographie et évolution dynamique, Doc. Lab. Geol. Fac. 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Santisteban, C. Taberner, Shallow marine and continental conglomerates derived fromcoral reef complexes after desiccation of a deep marine basin: the Tortonian-Messinian deposits of the Fortuna Basin SE, Spain, J.Geol. Soc. Lond. 140 (1983) 401–411. [25] J.M. Soria, P. Alfaro, J. Fernández, C. Viseras, Quantitative subsidence-uplift analysis of the Bajo Segura Basin (eastern Betic Cordillera, Spain): tectonic control on the stratigraphic architecture, Sediment Geol. 140 (2001) 271–289. [26] J.M. Soria, A. Yébenes, J.E. Caracuel, La sección Messiniense- Plioceno de Crevillente (Cordillera Bética oriental): expresión de la crisis de salinidad del Mediterráneo, Geogaceta 31 (2002) 159–162. [27] J.M. Soria, J.E. Tent-Manclús, J.E. Caracuel, A. Yébenes, C. Lancis, A. Estévez, La crisis de salinidad Tortoniense: su registro en la zona de enlace entre las cuencas de Fortuna y del Bajo Segura, Geo-Temas 8 (2005) 113–118. [28] J.E. Tent-Manclús, Estructura y estratigrafía de las sierras de Crevillente, Abanilla y Algayat: su relación con la Falla de Crevillente, doctoral dissertation, Universidad de Alicante, 2006. [29] J.E. Tent-Manclús, C. Lancis, J. Dinarès-Turell, A. Estévez, Primeros datos bioestratigráficos de los grupos evaporíticos de la Cuenca de Fortuna (Cordillera Bética), Geogaceta 41 (2007) 231–234. [30] J.E. Tent-Manclús, A. Yébenes, A. Estévez, ?Por qué son tan diferentes las sierras de Crevillente y Abanilla? Geogaceta 37 (2005) 71–74. [31] C. Viseras, J. M. Soria, J. Fernández, Cuencas neógenas postorogénicas de la Cordillera Bética, in: J.A. Vera (Ed.), Geología de España SGE-IGME, 2004, pp. 576–581.en
dc.description.obiettivoSpecifico2.2. Laboratorio di paleomagnetismoen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorTent-Manclús, J. E.en
dc.contributor.authorSoria, J. M.en
dc.contributor.authorEstévez, A.en
dc.contributor.authorLancis, C.en
dc.contributor.authorCaracuel, J. E.en
dc.contributor.authorDinarès-Turell, J.en
dc.contributor.authorYébenes, A.en
dc.contributor.departmentDepartamento de Ciencias de la Tierra y del Medio Ambiente, Universidad de Alicante, Apto. 99, 03080 San Vicente del Raspeig, Alicante, Spainen
dc.contributor.departmentDepartamento de Ciencias de la Tierra y del Medio Ambiente, Universidad de Alicante, Apto. 99, 03080 San Vicente del Raspeig, Alicante, Spainen
dc.contributor.departmentDepartamento de Ciencias de la Tierra y del Medio Ambiente, Universidad de Alicante, Apto. 99, 03080 San Vicente del Raspeig, Alicante, Spainen
dc.contributor.departmentDepartamento de Ciencias de la Tierra y del Medio Ambiente, Universidad de Alicante, Apto. 99, 03080 San Vicente del Raspeig, Alicante, Spainen
dc.contributor.departmentDepartamento de Ciencias de la Tierra y del Medio Ambiente, Universidad de Alicante, Apto. 99, 03080 San Vicente del Raspeig, Alicante, Spainen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.departmentDepartamento de Ciencias de la Tierra y del Medio Ambiente, Universidad de Alicante, Apto. 99, 03080 San Vicente del Raspeig, Alicante, Spainen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptDepartamento de Ciencias de la Tierra y del Medio Ambiente, Universidad de Alicante, Apdo. Correos 99, 03080 Alicante, Spain-
crisitem.author.deptUniversidad de Alicante, Departamento de Ciencias de la Tierra y del Medio Ambiente. Apto. 99. 03080 San Vicente del Raspeig. Alicante-
crisitem.author.deptUniversidad de Alicante, Departamento de Ciencias de la Tierra y del Medio Ambiente, Apto. 99, 03080 San Vicente del Raspeig, Alicante, Spain-
crisitem.author.deptUniversidad de Alicante, Departamento de Ciencias de la Tierra y del Medio Ambiente. Apto. 99. 03080 San Vicente del Raspeig. Alicante-
crisitem.author.deptUniversidad de Alicante, Departamento de Ciencias de la Tierra y del Medio Ambiente. Apto. 99. 03080 San Vicente del Raspeig. Alicante-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.deptUniversidad de Alicante, Departamento de Ciencias de la Tierra y del Medio Ambiente, Apto. 99, 03080 San Vicente del Raspeig, Alicante, Spain-
crisitem.author.orcid0000-0002-5546-2291-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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