Geochemistry of metasedimentary rocks from the Puncoviscana Complex in the Mojotoro Range, NW Argentina: Implications for provenance and tectonic setting
Low-grade metasedimentary rocks from the Lower Paleozoic Puncoviscana Complex of the Mojotoro Range in NW Argentina have been analyzed for their major and trace elements - including rare earth - in order to constrain their provenance and depositional tectonic setting. They show a moderate degree of...
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2017
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| LEADER | 22435caa a22014297a 4500 | ||
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| 001 | PAPER-25411 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518205727.0 | ||
| 008 | 190410s2017 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-85026528898 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Aparicio González, P.A. | |
| 245 | 1 | 0 | |a Geochemistry of metasedimentary rocks from the Puncoviscana Complex in the Mojotoro Range, NW Argentina: Implications for provenance and tectonic setting |
| 260 | |b Elsevier Ltd |c 2017 | ||
| 270 | 1 | 0 | |m Aparicio González, P.A.; INGEIS–CONICET Instituto de Geocronología y Geología Isotópica, Consejo Nacional de Investigaciones Científicas y Técnicas, Universidad de Buenos Aires, Ciudad UniversitariaArgentina; email: pamelaaparicio@gmail.com |
| 506 | |2 openaire |e Política editorial | ||
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| 520 | 3 | |a Low-grade metasedimentary rocks from the Lower Paleozoic Puncoviscana Complex of the Mojotoro Range in NW Argentina have been analyzed for their major and trace elements - including rare earth - in order to constrain their provenance and depositional tectonic setting. They show a moderate degree of chemical weathering with intermediate CIA (<75) values and can be classified as metawackes and metapelites. Provenance discrimination diagrams based on major element geochemistry and trace element ratios (i.e., Cr/V, Y/Ni, Th/Co, La/Sc, Th/Sc, Eu/Eu*) suggest that the sediments were derived from upper crustal, felsic source rocks. Tectonic setting discrimination diagrams based on major elements, immobile trace elements (i.e., La- Th- Sc and Th-Sc-Zr/10) and La/Yb vs. Eu/Eu* plots, support an active margin setting associated with a magmatic arc located to the east of the Neoproterozoic–Cambrian Pampean Brazilian arc that formed along the margin of a Mesoproterozoic craton. © 2017 |l eng | |
| 593 | |a INGEIS–CONICET Instituto de Geocronología y Geología Isotópica, Consejo Nacional de Investigaciones Científicas y Técnicas, Universidad de Buenos Aires, Ciudad Universitaria, Buenos Aires, C1428EHA, Argentina | ||
| 593 | |a Centro de Geoquímica, Instituto de Ciencias de la Tierra, Facultad de Ciencias, Universidad Central de Venezuela, Caracas, 38951010-A, Venezuela | ||
| 593 | |a Laboratory of Geochronology, Instituto de Geociências, Universidade de Brasília, Brasília, DF 70910 900, Brazil | ||
| 593 | |a Universidad Nacional de Salta, Salta, 3700, Argentina | ||
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