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DOI10.1130/B31892.1
Magnetobiochronology of Lower Pliocene marine sediments from the lower Guadalquivir Basin: Insights into the tectonic evolution of the Strait of Gibraltar area
Pérez-Asensio J.N.; Larrasoaña J.C.; Samankassou E.; Sierro F.J.; Garcia-Castellanos D.; Jiménez-Moreno G.; Salazar Á.; Salvany J.M.; Ledesma S.; Pilar Mata M.; Civis J.; Mediavilla C.
发表日期2018
ISSN167606
起始页码1791
结束页码1808
卷号130期号:2021-11-12
英文摘要The Gibraltar Arc is a complex tectonic region, and several competing models have been proposed to explain its evolution. We studied the sedimentary fill of the Guadalquivir Basin to identify tectonic processes that were occurring when the reopening of the Strait of Gibraltar led to the reestablishment of Mediterranean outflow. We present a chronostratigraphic framework for the Lower Pliocene sediments from the lower Guadalquivir Basin (SW Spain). The updated chronology is based on magnetobiostratigraphic data from several boreholes. Our results show that the studied interval in the La Matilla core is in the early Pliocene section, providing better constraints on the sedimentary evolution of the basin during that period. Migrating depositional facies led to a younger onset of sandy deposition basinward. At the northwestern passive margin, a 0.7 m.y. period of sedimentary bypass related to a sharp decrease in sedimentation rates and lower sea levels resulted from the tectonic uplift of the forebulge. In contrast, high sedimentation rates with continuous deep-marine sedimentation are recorded at the basin center due to continuous tectonic subsidence and west-southwestward progradation of axial depositional systems. The marginal forebulge uplift, continuous tectonic basinal subsidence, and southward progradation of clinoforms in the early Pliocene can be explained by the pull of a lithospheric slab beneath the Gibraltar Arc as the Strait of Gibraltar opened. These findings are, to our knowledge, the first reported sedimentary expression of slab pull beneath the Betics related to the opening of the Strait of Gibraltar after the Messinian salinity crisis. © 2018 Geological Society of America.
语种英语
来源期刊Bulletin of the Geological Society of America
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/184995
作者单位Department of Earth Sciences, University of Geneva, Rue des Maraîchers 13, Geneva, 1205, Switzerland; GRC Geociències Marines, Departament de Dinàmica de la Terra i de l'Oceà, Facultat de Ciències de la Terra, Universitat de Barcelona, Carrer Martí i Franquès s/n, Barcelona, 08028, Spain; Instituto Geológico y Minero de España, Unidad de Zaragoza, Manuel Lasala 44, Zaragoza, 50006, Spain; Institute of Earth Sciences Jaume Almera, Consejo Superior de Investigaciones Científicas, Carrer Solé i Sabarís s/n, Barcelona, 08028, Spain; Department of Geology, University of Salamanca, Salamanca, 37008, Spain; Departamento de Estratigrafía y Paleontología, Universidad de Granada, Fuente Nueva s/n, Granada, 18002, Spain; Instituto Geológico y Minero de España, La Calera 1, Tres Cantos, Madrid, 28760, Spain; Departament d'Enginyeria Civil i Ambiental, Universitat Politècnica de Catalunya, Carrer Jordi Girona 31, Barcelona, 08034, Spain; Gas Natural Fenosa, Avenida San Luis 77, Madrid, 28033, Spain; Instituto Geológic...
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Pérez-Asensio J.N.,Larrasoaña J.C.,Samankassou E.,et al. Magnetobiochronology of Lower Pliocene marine sediments from the lower Guadalquivir Basin: Insights into the tectonic evolution of the Strait of Gibraltar area[J],2018,130(2021-11-12).
APA Pérez-Asensio J.N..,Larrasoaña J.C..,Samankassou E..,Sierro F.J..,Garcia-Castellanos D..,...&Mediavilla C..(2018).Magnetobiochronology of Lower Pliocene marine sediments from the lower Guadalquivir Basin: Insights into the tectonic evolution of the Strait of Gibraltar area.Bulletin of the Geological Society of America,130(2021-11-12).
MLA Pérez-Asensio J.N.,et al."Magnetobiochronology of Lower Pliocene marine sediments from the lower Guadalquivir Basin: Insights into the tectonic evolution of the Strait of Gibraltar area".Bulletin of the Geological Society of America 130.2021-11-12(2018).
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