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  2. Geology of Brazil - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Brazil

    Formed between the Mesozoic and Cenozoic, Brazil has numerous offshore basins that contain oil, related to the rifting of the Atlantic Ocean. The Sergipe-Alagoas Basin is an example of Aptian age shale, conglomerate and sandstone deposited in the final phase of rifting, while the Miranga, Aracas, Dom Joao and Agua Grande fields reflect mid ...

  3. Brazilian Highlands - Wikipedia

    en.wikipedia.org/wiki/Brazilian_Highlands

    The Brazilian Highlands or Brazilian Plateau (Portuguese: Planalto Brasileiro) is an extensive geographical region covering most of the eastern, southern and central portions of Brazil, in all some 4,500,000 km 2 (1,930,511 sq mi) or approximately half of the country's land area.

  4. Sociedade Brasileira de Geologia - Wikipedia

    en.wikipedia.org/wiki/Sociedade_Brasileira_de...

    Sociedade Brasileira de Geologia (SBG) Other name (English: Brazilian Geological Society) Established: 6 May 1945: Mission "To foster the knowledge and development of geosciences, applied geology and related research and technology and the rational and sustainable use of mineral and water resources" [1]

  5. Category:Geology of Brazil - Wikipedia

    en.wikipedia.org/wiki/Category:Geology_of_Brazil

    This page was last edited on 26 October 2019, at 04:37 (UTC).; Text is available under the Creative Commons Attribution-ShareAlike 4.0 License; additional terms may apply.

  6. Geography of Brazil - Wikipedia

    en.wikipedia.org/wiki/Geography_of_Brazil

    In the north, a large area is occupied by the Amazonian lowland. To the south of it is the strongly dissected Brazilian lowland. Between the Brazilian lowland and the Atlantic Ocean is a narrow coastal lowland. Brazil has large deposits of oil, iron, bauxite, nickel, uranium, manganese ores, diamonds and other minerals.

  7. Amazonian Craton - Wikipedia

    en.wikipedia.org/wiki/Amazonian_craton

    The São Luís and Luis Alves cratonic fragments (Brazil) are shown, but the Arequipa–Antofalla Craton, the Sahara Craton, and some minor African cratons are not. Other versions describe the Guiana Shield separated from the Amazonian Shield by a depression.

  8. Paraná and Etendeka traps - Wikipedia

    en.wikipedia.org/wiki/Paraná_and_Etendeka_traps

    The basalt samples at Paraná and Etendeka have an age of about 132 Ma, during the Valanginian stage of the Early Cretaceous. [3] Indirectly, the rifting and extension are probably the origin of the Paraná and Etendeka traps and it could be the origin of the Gough and Tristan da Cunha Islands as well, as they are connected by the Walvis Ridge (Gough/Tristan hotspot).

  9. Brazilian Journal of Geology - Wikipedia

    en.wikipedia.org/wiki/Brazilian_Journal_of_Geology

    The journal covers the field of geology and related earth sciences, in Brazil, South America, and Antarctica, including oceanic regions adjacent to these regions. [1] The journal was established in 1971 and articles are published in English and Portuguese. The journal replaced the Boletim da Sociedade Brasileira de Geologia established in 1952.