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dc.contributor.authorCózar, Pedroes_ES
dc.contributor.authorSomerville, Ianes_ES
dc.contributor.authorVachard, Danieles_ES
dc.contributor.authorCoronado, Ismaeles_ES
dc.contributor.authorGarcía-Frank, Alejandraes_ES
dc.contributor.authorMedina-Varea, Paulaes_ES
dc.contributor.authorSaid, Ismaeles_ES
dc.contributor.authorMoral, Begoña deles_ES
dc.contributor.authorRodríguez, Sergioes_ES
dc.date.accessioned2019-06-20T06:41:20Z-
dc.date.available2019-06-20T06:41:20Z-
dc.date.issued2016-08-
dc.identifier.citationGondwana Research - International Geoscience Journal 36: 459-472 (2016)es_ES
dc.identifier.issn1342-937X-
dc.identifier.urihttp://hdl.handle.net/10261/184439-
dc.description.abstractRevision of several important Carboniferous stratigraphic successions in basins in the Saharan Platform allows us to propose distinct biostratigraphical boundaries for the upper Viséan, lower and upper Serpukhovian and lower Bashkirian, with the latter boundary separating upper Mississippian from lower Pennsylvanian strata. The boundaries are not only defined primarily by foraminifers but also incorporate ammonoid and conodont data. This study shows that the positioning of some boundaries differs significantly from previous studies in the region. For the studied interval, it can be recognized that two well-defined tectonic events were widespread in the entire Sahara Platform: a mostly late Viséan event and a latest Serpukhovian–early Bashkirian event. Both tectonic events show a marked tendency to become younger eastward, and they are compared to the intra-Viséan phase of the Variscan Orogeny and the main phase of this orogeny, respectively.es_ES
dc.description.sponsorshipFieldwork was funded by the Spanish Ministerio de Economía y Competitividad (research project CGL2012-30922BTE).es_ES
dc.language.isoenges_ES
dc.publisherElsevieres_ES
dc.rightsclosedAccesses_ES
dc.subjectBiostratigraphyes_ES
dc.subjectLate Mississippianes_ES
dc.subjectNorth Africaes_ES
dc.subjectSaharan basinses_ES
dc.subjectForaminiferses_ES
dc.titleUpper Mississippian to lower Pennsylvanian biostratigraphic correlation of the Sahara Platform successions on the northern margin of Gondwana (Morocco, Algeria, Libya)es_ES
dc.typeartículoes_ES
dc.identifier.doi10.1016/j.gr.2015.07.019-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttps://doi.org/10.1016/j.gr.2015.07.019es_ES
dc.contributor.funderMinisterio de Economía y Competitividad (España)es_ES
dc.relation.csices_ES
oprm.item.hasRevisionno ko 0 false*
dc.identifier.funderhttp://dx.doi.org/10.13039/501100003329es_ES
dc.contributor.orcidCoronado, Ismael [0000-0002-8469-6003]es_ES
dc.contributor.orcidGarcía-Frank, Alejandra [0000-0002-2350-002X]es_ES
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