U-Pb Ages and Hf Isotopes in Zircons from Parautochthonous Mesozoic Terranes in the Western Margin of Pangea: Implications for the Terrane Configurations in the Northern Andes

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dc.citation.journalTitleJOURNAL OF GEOLOGY
dc.contributor.authorBustamante C.
dc.contributor.authorArchanjo C.J.
dc.contributor.authorCardona A.
dc.contributor.authorBustamante A.
dc.contributor.authorValencia V.A.
dc.contributor.departmentUniversidad EAFIT. Departamento de Cienciasspa
dc.contributor.researchgroupGeología Ambiental y Tectónicaspa
dc.creatorBustamante C.
dc.creatorArchanjo C.J.
dc.creatorCardona A.
dc.creatorBustamante A.
dc.creatorValencia V.A.
dc.date.accessioned2021-03-26T21:25:56Z
dc.date.available2021-03-26T21:25:56Z
dc.date.issued2017-09-01
dc.description.abstractU-Pb laser ablation inductively coupled plasma mass spectrometry ages and Hf isotopes in zircons were used to constrain the nature of two geological units representative of the basement of the Central Cordillera of Colombia. Graphite-quartz-muscovite schists from the Cajamarca Complex show inherited detrital zircons supplied mostly from Late Jurassic (ca. 167 Ma), Ediacaran (ca. 638 Ma), and Tonian (Grenvillian; ca. 1000 Ma) sources. These marine volcanosedimentary deposits form an N-trending metamorphic belt in fault contact to the east with orthogneisses and amphibolites of the Tierradentro unit. Zircon U-Pb determinations of the Tierradentro rockspreviously interpreted as Grenvillian basement slicesyielded crystallization ages between 271 and 234 Ma. Initial Hf data reveal that the Tierradentro unit shares isotopic characteristics similar to other Permo-Triassic rocks of the Central Cordillera. In contrast, inherited detrital zircons from the Jurassic metasedimentary rocks suggest that their sources are distinct from the plutonic rocks that crop out in the Central Cordillera with Jurassic crystallization ages. Large xenoliths of the Tierradentro unit within the Ibague batholith indicate that the granodioritic magma mostly intruded a Permo-Triassic basement possibly by exploiting the Otu-Pericos fault. The Jurassic metasedimentary belt is correlated further south with a similar sequence in the Ecuadorian Andes named Salado terrane.eng
dc.identifierhttps://eafit.fundanetsuite.com/Publicaciones/ProdCientif/PublicacionFrw.aspx?id=7544
dc.identifier.doi10.1086/693014
dc.identifier.issn00221376
dc.identifier.issn15375269
dc.identifier.otherWOS;000408364800001
dc.identifier.otherSCOPUS;2-s2.0-85029482616
dc.identifier.urihttp://hdl.handle.net/10784/27238
dc.languageeng
dc.language.isoengeng
dc.publisherUNIV CHICAGO PRESS
dc.relation.urihttps://www.scopus.com/inward/record.uri?eid=2-s2.0-85029482616&doi=10.1086%2f693014&partnerID=40&md5=1cb7b40e377084ab2b640daf2cbef2ea
dc.rightshttps://v2.sherpa.ac.uk/id/publication/issn/0022-1376
dc.sourceJOURNAL OF GEOLOGY
dc.subjectAndeseng
dc.subjectlandmarkseng
dc.subjectgeo-routeeng
dc.subjectgeo-tourismeng
dc.subjectitineraries.eng
dc.titleU-Pb Ages and Hf Isotopes in Zircons from Parautochthonous Mesozoic Terranes in the Western Margin of Pangea: Implications for the Terrane Configurations in the Northern Andeseng
dc.typearticleeng
dc.typeinfo:eu-repo/semantics/articleeng
dc.typeinfo:eu-repo/semantics/publishedVersioneng
dc.typepublishedVersioneng
dc.type.localArtículospa

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