Comparação entre o Complexo Juiz de fora e a Unidade Granulítica Ponte de Zinco: geocronologia U-Pb em zircão (LA-ICPMS), geoquímica isotópica e composição das fontes geradoras

• Autor(a) principal: André, Jefferson Lima Fernandes
• Data de Publicação: 2014
• Tipo de documento: Tese
• Idioma: por
• Título da fonte: Biblioteca Digital de Teses e Dissertações da UERJ
• Texto Completo: http://www.bdtd.uerj.br/handle/1/7007
• topic: Ponte de Zinco Granulite Unit; Juiz de Fora Complex; U-Pb geochronology; Isotopic geochemistry; Unidade Granulítica Ponte de Zinco; Complexo Juiz de Fora; Geocronologia U-Pb; Geoquímica isotópica; CNPQ::CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::GEOLOGIA::GEOQUIMICA

The comparison between the Juiz de Fora Complex JFC and the Ponte de Zinco Granulite Unit, (Mangaratiba RJ) has shown that there are some significant differences between those two units. At the Ponte de Zinco Granulite Unit, one can find ortogranulites with a granitic and granodioritic composition, this is embasement of the area, call here as Ribeirão das Lajes Ortogranulites. Two other ortoderived litotypes have also been found: (i) a orthogneiss with garnet, (MAN-JEF-03a), being that the garnet exists in a subordinated form; (ii) leucocratic orthogneiss, (MAN-JEF-04), with mylonitic characteristics. In addition to the latter, Metasedimentary rocks also spring up in the Unit. It has been interpreted that an organulite (MAN-JEF-01a) of a high-K, with a monzogranitic composition, has crystallized into ca. of 2653 ± 37 Ma (U-Pb into zircon by LA-ICPMS), affected by a Neoproterozoic event generated biotite, hornblende and overgrowth rims on zircon grains. Its model age of Nd of 2,7 Ga and its positive εNd of + 2,1, indicates a genesis from the depleted mantle, having assimilated of the crust, as zircon grains have been found of approximately 2996 ± 17 Ma and 3343 ± 3.8 Ma. The data of litogeochemistry and its ratio 87Sr/86Sr(t) (0,70529), are compatible with a generation in a continental arc. The orthogneiss with garnet (MAN-JEF-03a) has a granodioritic composition. Its crystallizing age, as interpreted by geocronological analysis U-Pb on zircon (LA-ICPMS), was ca. of 2117 ± 15 Ma. This litotype has been metamorphized on the Neoproterozoic, with an age of 631 ± 40 Ma being obtained at the lower intercept. Its isotopic data indicates a young rock generated from the mantle (TDM = de 2,1 Ga e εNd = +3,4), its high ratio 87Sr/86Sr(t) (0,710), together with the inherited zircon grains (2,6 Ga) and the presence of an enclave, indicate the assimilation of crusty rocks. The leucocratic orthogneiss, (MAN-JEF-04) classified as high-K, possesses a monzogranitic composition, age 2132 ± 9,4 Ma U-Pb on zircon (LA-ICPMS). One single grain of orthopyroxene found on lamina, which has been practically consumed by retrometamorphism, which might have happened in two moments, 647 ± 18 Ma and 595 ± 38 Ma, calculated through the age concordia, on homogeneous overgrowth and, by the lower intercept, respectively. Its low ratio 87Sr/86Sr(t) (0,0703) associated to the positive εNd (+2,3) and its model age of approximately 2,1 Ga, reveal that the rock was formed by a young mantle material. Now the geochronological analysis in U-Pb on zircon (LA- ICPMS) in the Juiz de Fora (MG) region, revealed the existence of two litotypes (Arqueanos): one ortogranulite granodioritic (MB-EF-01b), of low-K with an age of 2849 ± 11 Ma and a heritage of 2975 ± 10 Ma. Its e Nd positive (+5,9) indicates a genesis from the depleted mantle, but its high ratio 87Sr/86Sr(t) (0,709) indicates contamination of Rb from external sources, maybe caused by the crust assimilation, as the inherited zircons reveal and/or the retrometamorfic fluids. One other lipotype is a gabbroic of the type E-MORB, its age has been calculated in 2691 ± 14 Ma, with a retrometamorphism that occurred in the interval of 604 ± 67 Ma, obtained by the lower intercept. Its εNd equal to +3,4 and its ratio 87Sr/86Sr(t) (0,701) show the extraction from the depleted mantle. New isotopic data of CJF in the Três Rios (RJ) and Juiz de Fora (MG) regions, suggest that the calcium-alkaline ortogranulites may represent distinctive groups. There are rocks with positive εNd, which are associated to the depleted mantle, however rocks with negative εNd must have been generated by crustal fusion, which can be the fusion of the lower crust, due to the ratio 87Sr/86Sr(t) (0,70514) found in the sample MB-JEF-02a (ortogranulite of high-K) or mixture between the mantle and the crust. The basic ortogranulites possess positive εNd with low ratio 87Sr/86Sr(t), which indicates the extraction from the depleted mantle, nevertheless its ratio La/YbN and La/NbN higher than 1, reveal some contribution from an enriched source, as well as its ratio Pb/Pb, which is bigger than the ones calculated for the evolvement of Pb on Earth. These interpretations can still be extended to an alkaline metabasic, found in the Três Rios (RJ) region