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dc.contributor.authorVinyoles, Andreues_ES
dc.contributor.authorLópez-Blanco, M.es_ES
dc.contributor.authorGarcés, Migueles_ES
dc.contributor.authorArbués, P.es_ES
dc.contributor.authorValero, Luises_ES
dc.contributor.authorBeamud, Elisabetes_ES
dc.contributor.authorOliva-Urcia, Belénes_ES
dc.contributor.authorCabello, Patriciaes_ES
dc.date.accessioned2020-08-19T12:42:39Z-
dc.date.available2020-08-19T12:42:39Z-
dc.date.issued2021-
dc.identifier.citationBasin Research,33(1): 447-477 (2021)es_ES
dc.identifier.issn0950-091X-
dc.identifier.urihttp://hdl.handle.net/10261/218253-
dc.description.abstractThe propagation of the deformation front in foreland systems is typically accompanied by the incorporation of parts of the basin into wedge-top piggy-back basins, this process is likely producing considerable changes to sedimentation rates (SR). Here we investigate the spatial-temporal evolution of SR for the Tremp–Jaca Basin in the Southern Pyrenees during its evolution from a wedge-top, foreredeep, forebulge configuration to a wedge-top stage. SR were controlled by a series of tectonic structures that influenced subsidence distribution and modified the sediment dispersal patterns. We compare the decompacted SR calculated from 12 magnetostratigraphic sections located throughout the Tremp–Jaca Basin represent the full range of depositional environment and times. While the derived long-term SR range between 9.0 and 84.5 cm/kyr, compiled data at the scale of magnetozones (0.1–2.5 Myr) yield SR that range from 3.0 to 170 cm/kyr. From this analysis, three main types of depocenter are recognized: a regional depocenter in the foredeep depozone; depocenters related to both regional subsidence and salt tectonics in the wedge-top depozone; and a depocenter related to clastic shelf building showing transgressive and regressive trends with graded and non-graded episodes. From the evolution of SR we distinguish two stages. The Lutetian Stage (from 49.1–41.2 Ma) portrays a compartmentalized basin characterized by variable SR in dominantly underfilled accommodation areas. The markedly different advance of the deformation front between the Central and Western Pyrenees resulted in a complex distribution of the foreland depozones during this stage. The Bartonian–Priabonian Stage (41.2–36.9 Ma) represents the integration of the whole basin into the wedge-top, showing a generalized reduction of SR in a mostly overfilled relatively uniform basin. The stacking of basement units in the hinterland during the whole period produced unusually high SR in the wedge-top depozone. © 2020 The Authors. Basin Research © 2020 John Wiley & Sons Ltd, European Association of Geoscientists & Engineers and International Association of Sedimentologistses_ES
dc.description.sponsorshipAgència de Gestió d'Ajuts Universitaris i de Recerca, Grant/Award Number: 2017SGR596; Secretaría de Estado de Investigación, Desarrollo e Innovación, Grant/Award Number: BES-2015-073302 and CGL2014-55900-P; Swiss National Science Foundation, Grant/Award Number: 200020_182017es_ES
dc.language.isoenges_ES
dc.publisherJohn Wiley & Sonses_ES
dc.relationMINECO/ICTI2013-2016/CGL2014-55900-Pes_ES
dc.rightsopenAccessen_EN
dc.subjectTremp–Jaca basines_ES
dc.subjectsedimentation–tectonicses_ES
dc.subjectssediment routing systemes_ES
dc.subjectsalt tectonices_ES
dc.subjectmagnetostratigraphyes_ES
dc.subjectEocenees_ES
dc.subjectdecompacted sedimentation rateses_ES
dc.title10 Myr evolution of sedimentation rates in a deep marine to non‐marine foreland basin system: Tectonic and sedimentary controls (Eocene, Tremp–Jaca Basin, Southern Pyrenees, NE Spain)es_ES
dc.typeartículoes_ES
dc.identifier.doi10.1111/bre.12481-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttps://doi.org/10.1111/bre.12481es_ES
dc.rights.licensehttps://creativecommons.org/licenses/by/4.0/-
dc.contributor.funderGeneralitat de Catalunyaes_ES
dc.contributor.funderMinisterio de Economía y Competitividad (España)es_ES
dc.contributor.funderSwiss National Science Foundationes_ES
dc.relation.csices_ES
oprm.item.hasRevisionno ko 0 false*
dc.identifier.funderhttp://dx.doi.org/10.13039/501100002809es_ES
dc.identifier.funderhttp://dx.doi.org/10.13039/501100003329es_ES
dc.contributor.orcidBeamud, Elisabet [0000-0003-3158-2966]es_ES
item.grantfulltextopen-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
item.openairetypeartículo-
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