EM - Escola de Minas
URI permanente desta comunidadehttp://www.hml.repositorio.ufop.br/handle/123456789/6
Notícias
A Escola de Minas de Ouro Preto foi fundada pelo cientista Claude Henri Gorceix e inaugurada em 12 de outubro de 1876.
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3 resultados
Resultados da Pesquisa
Item Rhyacian magmatic arc rocks with sanukitoid geochemical signature from the Juiz de Fora Complex, Minas-Bahia Orogenic System (SE-Brazil).(2022) Ferreira, Sandro Lúcio Mauri; Heilbron, Monica da Costa Pereira Lavalle; Bruno, Henrique; Marques, Rodson de Abreu; Neto, Carla; Valeriano, Claudio de Morisson; Bersan, Samuel Moreira; Romero, Luiz Felipe; Geraldes, Mauro CésarSanukitoid rocks make up a complete magmatic series with distinct geochemical characteristics of TTG suites and granitoids from modern magmatic arcs and are regarded as markers of the transition from typically Archean geodynamics to modern plate tectonics. Although most known sanukitoid suites formed during the Neoarchean and Mesoarchean, numerous papers have characterized Paleoproterozoic magmatic arc granitoid rocks showing affinity with the sanukitoid series. This work presents new data from field, lithogeochemistry, zircon U-Pb geochronology, and Sm-Nd and Sr isotopic studies on granodioritic granulites with sanukitoid signatures from the Juiz de Fora Complex (JFC), one of the Paleoproterozoic tectonic components of the Minas-Bahia Orogenic System (MBOS), southern São Francisco Paleocontinent (southeastern Brazil). These rocks crystallized at ~2175 Ma and present values of εNdt between −4.0 and +0.5, TDM between 2.57 and 2.12 Ga, and 87Sr/86Sri between 0.6937 and 0.7137. We interpret these rocks as the result of crystallization of magmas from a hybrid mantle source extensively contaminated by crustal material during protracted subduction. In southeastern São Francisco Paleocontinent, the association of sanukitoid rocks with other magmatic arc rocks points to a complex and prolonged Rhyacian accretionary system similar to modern plate tectonics.Item New clues for magma-mixing processes using petrological and geochronological evidence from the Castelo Intrusive Complex, Araçuaí Orogen (SE Brazil).(2022) Macêdo, Iago Mateus Lopes de; Geraldes, Mauro César; Marques, Rodson de Abreu; Melo, Marilane Gonzaga de; Tavares, Armando Dias; Martins, Maria Virgínia Alves; Oliveira, Hudson Costa; Rodrigues, Renzo DiasBimodal magmatism was recorded during the post-collisional stage that occurred during the Brasiliano/Pan-African cycle in the Araçuaí Orogen (southeastern Brazil) at ∼500 Ma. The Castelo Intrusive Complex (CIC) is a zoned post-collisional pluton in the orogen and is composed of monzogranites, granodiorites, quartz monzodiorites and diorites. CIC (∼100 km2) was emplaced along a regional lineament during the post-collisional stage of the orogeny and cut pre-collisional granitoids and metasedimentary sequences. In this work, a detailed petrographic study associated with data on U–Pb ages and Hf isotopic compositions of zircons from monzogranites, quartz monzodiorites and leucocratic dikes is presented to detail the geochronology, composition and context of CIC emplacement. Macroscale and microscale records show that several CIC lithotypes demonstrate the direct interaction of contemporaneous felsic and mafic magmas. U–Pb age dating of zircons (by laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS)) reveal crystallization ages of 486 ± 6 Ma for quartz monzodiorites and 524 ± 5 Ma to 499 ± 4 Ma for monzogranites. The analyzed leucocratic dike at 426 ± 15 Ma represents a late magmatic pulse. Hafnium isotopic data show variable ƐHf(t) values (from −24.05 to +12.7) and depleted mantle model ages (TDM) of 2.71–0.64 Ga, indicating the involvement of distinctly different mantle and crustal sources. At least two crustal sources with different Hf isotope signatures were distinguished (TDM of 2.6–2.4 Ga and ƐHf(t) of −26 to −22; and TDM of 2.2–1.7 Ga and ƐHf(t) of −17 to −8). These results suggest that the rocks in this study were partially derived from Archean and Paleoproterozoic crust. The isotopic data also show TDM model ages ranging from 1.28 to 0.64 Ga, with highly positive ƐHf(t) values (from +1.6 to +12.7). These data suggest the existence of a mantle reservoir source for magma generation and for heat that induced crustal melting during the post-collisional stage of the Araçuaí Orogen.Item Multiple processes of geochemical evolution for the alkaline rocks of Rio Bonito intrusive complex, Rio de Janeiro State, Brazil : 40Ar/39Ar and U-Pb ages and Lu-Hf isotopes on zircon and constraints on crustal signature.(2020) Silva, Daniel Adelino da; Motoki, Akihisa; Santos, Anderson Costa dos; Mendes, Julio; Jourdan, Fred; Geraldes, Mauro César; Lana, Cristiano de CarvalhoThis article presents geochemical characteristics of the alkaline rocks of Rio Bonito intrusive complex, State of Rio de Janeiro, Brazil, which is constituted mainly by nepheline syenite. The fractional crystallisation of this magma decreases K2 O/(Na2 O + K2 O) and increases (Na + K)/Al. The TiO2 , Fe2 O3 *, MgO, CaO, and P2 O5 contents indicate fractionation of titanite, ilmenite, and clinopyroxene or amphibole. The total rare earth elements (REEs) are high, and the REE pattern is linear with negative gradient. The nepheline syenite aplite has low REEs, concave REE pattern, and positive Eu anomaly. The ultrabasic and basic mela-nepheline syenite samples have total REEs and light REEs higher than the felsic alkaline rocks. Therefore, the nepheline syenite magma is not derived directly from the alkaline ultrabasic magma. Laser-spot step-heating 40Ar/39Ar ages for biotite and amphibole are 65.03 ± 0.70 and 65.03 ± 0.46. U-Pb ages LA-ICP-MS for two samples are 65.49 ± 0.30 and 65.18 ± 0.30. Values of εHf are negative for both samples, indicating an important crustal component in the evolution of Rio Bonito.