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Mostrando ítems 1-10 de 41
THE MANTIQUEIRA PROVINCE: ARCHEAN STRUCTURE AND PROTEROZOIC EVOLUTIONTHE MANTIQUEIRA PROVINCE: ARCHEAN STRUCTURE AND PROTEROZOIC EVOLUTION
(Sociedade Brasileira de Geologia, 2018)
NEOPROTEROZOIC GRANITOID SUITES IN SOUTHEASTERN BRAZILNEOPROTEROZOIC GRANITOID SUITES IN SOUTHEASTERN BRAZIL
(Sociedade Brasileira de Geologia, 2017)
Neoproterozoic evolution of the basement of the South-American platform
(Oxford, 2013)
Neoproterozoic geologic and geotectonic processes were of utmost importance in forming and structuring
the basement framework of the South-American platform. Two large domains with distinct
evolutionary histories are ...
Morphostructural compartments of the Itapemirim River Catchment, in the southern region of the State of Espírito Santo, BrazilCompartimentação morfoestrutural da Bacia Hidrográfica do Rio Itapemirim, sul do estado do Espírito Santo
(Universidade de São Paulo, Instituto de Geociências, 2018)
Structural context of the guapiara topographic map areaContexto estrutural da área da folha topográfica guapiara
(2018-01-01)
The Guapiara Topographic Map 1:50,000 is located in the southernmost part of the state of São Paulo and comprises the northern portion of the Apiaí Terrain, of meso-to neoproterozoic age, inserted in the central-southern ...
Filogenia molecular de Brucepattersonius (Sigmodontinae: Akodontini) com uma análise morfométrica craniana do gênero
(Universidade Federal do Rio de JaneiroBrasilMuseu NacionalPrograma de Pós-Graduação em Ciências Biológicas (Zoologia)UFRJ, 2017)
Geology of guapiara topographic sheet in 1:50.000.Geologia da folha topográfica guapiara na escala 1:50.000.
(2018-01-01)
Geology of Guapiara Topographic Sheet in 1:50.000. The region of Guapiara Topographic Sheet is located in the extreme South of the São Paulo state and it is comprised in the central portion of the Mantiqueira Province in ...
Contribution of SHRIMP U-Pb zircon geochronology to unravelling the evolution of Brazilian Neoproterozoic fold belts
(ELSEVIER SCIENCE BV, 2010)
The South-American continent is constituted of three major geologic-geotectonic entities the homonym platform (consolidated at the end of the Cambrian) the Andean chain (essentially Meso-Cenozoic) and the Patagonian terrains ...