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Hildor José Seer

Researcher at Centro Federal de Educação Tecnológica de Minas Gerais

Publications -  21
Citations -  466

Hildor José Seer is an academic researcher from Centro Federal de Educação Tecnológica de Minas Gerais. The author has contributed to research in topics: Craton & Terrane. The author has an hindex of 10, co-authored 21 publications receiving 412 citations. Previous affiliations of Hildor José Seer include Universidade Tecnológica Federal do Paraná, Medianeira.

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U-Pb geochronology of the southern Brasília belt (SE-Brazil): Sedimentary provenance, Neoproterozoic orogeny and assembly of West Gondwana

TL;DR: In this paper, the authors reported new U-Pb data from the southern sector of the Brasilia belt in order to provide temporal limits for the deposition and ages of provenance of sediments accumulated in passive margin successions around the south and southwestern margins of the Sao Francisco Craton, and date the orogenic events leading to the amalgamation of West Gondwana.
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The kamafugite-carbonatite association in the alto paranaíba igneous province (apip) southeastern brazil

TL;DR: The Late-Cretaceous Alto Paranaiba Igneous Province (APIP) comprises a variety of ultrapotassic rock types, including kimberlites, lamproites and large volumes of kamafugites, in addition to a number of carbonatite-bearing plutonic alkaline complexes as mentioned in this paper.
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Grupo araxá em sua área tipo: um fragmento de crosta oceânica neoproterozóica na faixa de dobramentos brasília

TL;DR: In this article, the authors present a new evolution model for the Araxa Group in its type area, the southern segment of the Neoproterozoic Brasilia Belt, Minas Gerais, Brazil.
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Provenance shift from a continental margin to a syn-orogenic basin in the Neoproterozoic Araxá nappe system, southern Brasília belt, Brazil

TL;DR: In the southern Brasilia belt of central Brazil, prominent east-verging systems of stacked nappes caused the thrusting and tectonic interleaving of metasedimentary rocks of different provenance, age and metamorphism as discussed by the authors.