Ediacaran
Mostrando 1-12 de 24 artigos, teses e dissertações.
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1. O Que Faz um Artigo ser Mais Citado?
Abstract The Guacuí and Batatal lineaments in the southern region of the state of Espírito Santo (southeastern Brazil) can be traced from satellite images for tens of kilometers. They are considered shear zones associated to the final tectonic stages of the Araçuaí-West Congo (A-WC) Orogen during the Ediacaran-Cambrian period. In order to understand thei
Rev. adm. contemp.. Publicado em: 2020-12
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2. Structure and tectonic significance of high- and low-temperature deformation along the lateral escape-related Guaçuí and Batatal shear zones, southern Araçuaí Orogen (southeastern Brazil)
Abstract The Guacuí and Batatal lineaments in the southern region of the state of Espírito Santo (southeastern Brazil) can be traced from satellite images for tens of kilometers. They are considered shear zones associated to the final tectonic stages of the Araçuaí-West Congo (A-WC) Orogen during the Ediacaran-Cambrian period. In order to understand thei
REM, Int. Eng. J.. Publicado em: 2020-12
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3. Ediacaran emerald mineralization in Northeastern Brazil: the case of the Fazenda Bonfim Deposit
Abstract The Fazenda Bonfim emerald deposit lies within the Seridó Belt. It is a classic example of deposit formed through metasomatic interactions between Be-rich granite intrusions and Cr(± V)-rich mafic-ultramafic rocks. The setting of the emerald mineralization was built under strong strike-slip dynamics, which produced serpentinization and talcificati
Braz. J. Geol.. Publicado em: 13/01/2020
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4. Provenance of the Ediacaran Salinas Formation (Araçuaí Orogen, Brazil): Clues from lithochemical data and zircon U-Pb (SHRIMP) ages of volcanic clasts
Abstract Salinas Formation occurs in a large region of the Northern Araçuaí orogen, Southeastern Brazil. It includes turbiditic wackes (> 10% matrix) to arenites (< 10% matrix), pelites and clast-supported conglomerates, metamorphosed from the biotite zone of the greenschist facies to the sillimanite zone of the amphibolite facies. Salinas Formation lies u
Braz. J. Geol.. Publicado em: 01/07/2019
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5. Depicting the 3D geometry of ore bodies using implicit lithological modeling: An example from the Horto-Baratinha iron deposit, Guanhães block, MG
Abstract The definition of geological domains is essential for mineral exploration and is traditionally done manually, section by section, in a laborious, time consuming and subjective process, to construct a 3D model. The technique referred to as implicit modeling is an option to model deposits in a fast and practical manner. This article presents the litho
REM, Int. Eng. J.. Publicado em: 19/06/2019
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6. Sedimentary provenance in the southern sector of the São Francisco Basin, SE Brazil
ABSTRACT: We present new Sm-Nd, U-Pb and Hf isotope geochronological data for the siliciclastic rocks in the southern sector of the São Francisco Basin. An abrupt change in the Sm-Nd data is observed from the Carrancas Formation’s oligomitic conglomerates (TDM ages between 2.7 and 3.3 Ga; εNd(550 Ma) values between -25.09 and -17.98), its finer facies, a
Braz. J. Geol.. Publicado em: 2018-01
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7. Acritarchs of the Ediacaran Frecheirinha Formation, Ubajara Group, Northeastern Brazil
We report for the first time the occurrence of organic-walled microfossils in Ediacaran limestones and marls of the Frecheirinha Formation, Ubajara Group, and the first Precambrian acritarchs so far reported for northeastern Brazil. The assemblage of the Frecheirinha Formation represents a low-diversity microflora comprising Leiosphaeridia, Lophosphaeridium
An. Acad. Bras. Ciênc.. Publicado em: 2015-06
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8. First evidence of the Ediacaran fauna in Northeastern Brazil, an albino dolphin, and trophic groups of a bird community in Alagoas
An. Acad. Bras. Ciênc.. Publicado em: 2014-09
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9. First Ediacaran Fauna Occurrence in Northeastern Brazil (Jaibaras Basin, ?Ediacaran-Cambrian): Preliminary Results and Regional Correlation
Este estudo relata a primeira ocorrência da fauna Ediacarana no Nordeste do Brasil (Município de Pacujá, noroeste do Estado do Ceará) e apresenta interpretações preliminares de seu significado. A correlação regional indica que os fósseis se originaram na Bacia do Jaibaras e que podem representar um novo sistema geológico. O ambiente de deposição
An. Acad. Bras. Ciênc.. Publicado em: 15/08/2014
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10. A influência da evolução de altos estruturais em sucessões aluviais: exemplos do Ediacarano e do Cambriano da Bacia Camaquã (RS) / The influence of the evolution of structural highs in alluvial successions: examples from the Ediacaran and from the Cambrian of the Camaquã Basin (Southern Brazil)
Análises de proveniência sedimentar são tradicionalmente utilizadas com o objetivo de reconstruir a relação entre depósitos sedimentares e suas respectivas áreas fonte, de forma a permitir a composição do contexto tectônico regional. Uma aplicação menos explorada dos métodos de análise de proveniência sedimentar é a avaliação detalhada das
Publicado em: 2010
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11. Quimioestratigrafia isotópica (C, O, S e Sr), geocronologia (Pb-Pb e K-Ar) e proveniência (Sm-Nd) das rochas da Faixa Paraguai Norte, Mato Grosso / Isotope (C, O, S And Sr) chemostratigraphy, geochronology (Pb-Pb And K-Ar) and provenance (Sm-Nd) of rocks from the North Paraguay Belt, Mato Grosso
Anomalias biogeoquímicas expressivas têm sido reconhecidas em rochas marinhas neoproterozoicas depositadas em todos os continentes, não havendo similares ao longo do Fanerozoico. O interesse nesta Era aumentou nos últimos anos, especialmente em relação ao Ediacarano, período que precede a grande Explosão de Vida Cambriana e que abriga os primeiros or
Publicado em: 2010
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12. Tectônica e sedimentação na Bacia do Camaquã Central (RS): exemplos do Grupo Guaritas e do Grupo Santa Bárbara / Tectonics and sedimentation in Central Camaquã Basin: the Guaritas Group and the Santa Bárbara Group
The relationship between tectonics and sedimentation plays a primordial role in the understanding of sedimentary successions. On the other hand, the study of pre-Silurian fluvial deposits represents a challenge due to the lack of interaction between land plants and river systems which characterizes post-Silurian environments. The Camaquã Basin (Ediacaran to
Publicado em: 2010