Geochemistry of Neoproterozoic-Cambrian metasedimentary rocks of the Caucete Group, Sierra de Pie de Palo, Argentina: Implications for their provenance

The Caucete Group is a low-grade metasedimentary sequence of probable late Neoproterozoic-Cambrian age. It is exposed on the western flank of the Sierra de Pie de Palo, a basement block of the Cuyania terrane from western Argentina. The geochemical composition (major, trace and rare-earth elements,...

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Autor principal: Naipauer, M.
Otros Autores: Cingolani, C.A, Vujovich, G.I, Chemale Jr., F.
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Publicado: 2010
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100 1 |a Naipauer, M. 
245 1 0 |a Geochemistry of Neoproterozoic-Cambrian metasedimentary rocks of the Caucete Group, Sierra de Pie de Palo, Argentina: Implications for their provenance 
260 |c 2010 
270 1 0 |m Naipauer, M.; Laboratorio de Tectónica Andina, Depto. de Ciencias Geológicas, FCEyN, Universidad de Buenos Aires, Pabellón II, Ciudad Universitaria, 428-Buenos Aires, Argentina; email: maxinaipauer@gl.fcen.uba.ar 
506 |2 openaire  |e Política editorial 
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520 3 |a The Caucete Group is a low-grade metasedimentary sequence of probable late Neoproterozoic-Cambrian age. It is exposed on the western flank of the Sierra de Pie de Palo, a basement block of the Cuyania terrane from western Argentina. The geochemical composition (major, trace and rare-earth elements, and Sm-Nd isotopes) of the El Quemado, La Paz, El Desecho, and Angacos formations (Caucete Group) was used to characterize the sedimentary provenance. We recognized two types of sources: A felsic source (crustal signature) and another mafic source with juvenile signature. Provenance is interpreted to be the mixing between Paleoproterozoic felsic rocks and Mesoproterozoic-Neoproterozoic juvenile rocks sources. This is supported by previous geochronological studies. The Cuyania basement is interpreted to be the Mesoproterozoic and Neoproterozoic juvenile component defined in the Caucete Group (e.g.: ophiolite assemblage of Sierra de Pie de Palo). The Cuyania basement is also considered to be the felsic source (paragneisses and meta-greywackes of the Pie de Palo Complex). We do not consider Gondwana as a provenance source based on the discrepancies in the Sm-Nd isotopic signatures and the detrital zircon provenance ages between the Caucete Group and the surrounding units that are considered to be autochthonous to the southern margin of Gondwana. The Caucete Group Laurentian Sm-Nd isotopic signature suggests that this sector could have been part of the source area. Hence an allochthonous origin for the Caucete Group (Cuyania terrane), derived from southern Laurentia, is supported for the geochemical results presented in this contribution. © 2010 Elsevier Ltd.  |l eng 
536 |a Detalles de la financiación: CONICET-PIP 5437, PICT 07-10829, PIP 5027 
536 |a Detalles de la financiación: Agencia Nacional de Promoción Científica y Tecnológica 
536 |a Detalles de la financiación: Fieldwork was partially financed by CONICET PIP 5027 , CONICET-PIP 5437 , and by PICT 07-10829 from ANPCYT (Argentina). The Centro de Investigaciones Geológicas (CIG-La Plata, Argentina) facilitated the use of their laboratories. We thank SPECTRAU, the Central Analytical Facility (University of Johannesburg, South Africa), for some XRD analyses. We also thank to the staff of the LGI-UFRGS, Porto Alegre, Brazil, particularly Prof. Dr. K. Kawashita for their scientific assistance. Dr. Patricia Dickerson, Paulina Abre, and Monica Escayola are thanked for their comments and suggestions in the final version of the manuscript. Finally, we are very grateful to reviewers Miguel Haller (Universidad Nacional de la Patagonia) and Heinrich Bahlburg (Westfälische Wilhelms-Universität) for their valuable comments and suggestions about the sedimentary geochemical aspects. 
593 |a Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET), Argentina 
593 |a Laboratorio de Tectónica Andina, Depto. de Ciencias Geológicas, FCEyN, Universidad de Buenos Aires, Pabellón II, Ciudad Universitaria, 1428-Buenos Aires, Argentina 
593 |a Centro de Investigaciones Geológicas, FCNyM, Universidad Nacional de La Plata, calle 1 N0 644, La Plata, Argentina 
593 |a Núcleo de Geociências, Universidade Federal do Sergipe, Brazil 
690 1 0 |a CAUCETE GROUP 
690 1 0 |a CUYANIA TERRANE 
690 1 0 |a LITHOGEOCHEMISTRY 
690 1 0 |a ND ISOTOPIC COMPOSITION 
690 1 0 |a PROVENANCE 
690 1 0 |a CAMBRIAN 
690 1 0 |a GEOCHEMISTRY 
690 1 0 |a ISOTOPIC COMPOSITION 
690 1 0 |a METASEDIMENTARY ROCK 
690 1 0 |a NEODYMIUM ISOTOPE 
690 1 0 |a PROTEROZOIC 
690 1 0 |a PROVENANCE 
690 1 0 |a RARE EARTH ELEMENT 
690 1 0 |a TRACE ELEMENT 
690 1 0 |a SIERRA DE PIE DE PALO 
690 1 0 |a SIERRAS PAMPEANAS 
651 4 |a ARGENTINA 
651 4 |a SAN JUAN [ARGENTINA] 
700 1 |a Cingolani, C.A. 
700 1 |a Vujovich, G.I. 
700 1 |a Chemale Jr., F. 
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