Antônio Carlos Pedrosa-Soares spends much of his time researching Geochemistry, Craton, Paleontology, Zircon and Rift. His Geochemistry research includes elements of Proterozoic, Granulite, Metamorphic facies and Plutonism. His Metamorphic facies research integrates issues from Tonian and Mafic.
Antônio Carlos Pedrosa-Soares interconnects Metamorphism, Back-arc basin and Oceanic crust in the investigation of issues within Craton. Antônio Carlos Pedrosa-Soares regularly ties together related areas like Basement in his Zircon studies. Rift is the subject of his research, which falls under Geomorphology.
Antônio Carlos Pedrosa-Soares mainly investigates Geochemistry, Zircon, Paleontology, Geomorphology and Mineralogy. Antônio Carlos Pedrosa-Soares has included themes like Back-arc basin, Basement and Pluton in his Geochemistry study. Antônio Carlos Pedrosa-Soares combines subjects such as Orosirian, Rhyacian and Archean with his study of Basement.
His Zircon research incorporates elements of Gondwana, Provenance, Craton and Geochronology. In his research, Banded iron formation is intimately related to Rift, which falls under the overarching field of Craton. His study looks at the relationship between Mineralogy and fields such as Schist, as well as how they intersect with chemical problems.
His scientific interests lie mostly in Geochemistry, Zircon, Tonian, Gondwana and Back-arc basin. As part of his studies on Geochemistry, Antônio Carlos Pedrosa-Soares often connects relevant areas like Granulite. His research in Zircon intersects with topics in Craton, Gneiss, Provenance and Statherian.
His research investigates the link between Craton and topics such as Suture that cross with problems in Ophiolite. In Tonian, Antônio Carlos Pedrosa-Soares works on issues like Orosirian, which are connected to Stenian, Rhyacian and Archean. His studies examine the connections between Back-arc basin and genetics, as well as such issues in Arc system, with regards to Basalt.
Geochemistry, Zircon, Gondwana, Back-arc basin and Metamorphism are his primary areas of study. He has researched Geochemistry in several fields, including Rhyacian and Craton. His Rhyacian study combines topics from a wide range of disciplines, such as Basement, Archean and Continental crust, Crust.
His studies deal with areas such as Orosirian, Felsic, Mafic and Statherian as well as Zircon. The concepts of his Gondwana study are interwoven with issues in Rift and Syncline. The various areas that Antônio Carlos Pedrosa-Soares examines in his Metamorphism study include Nappe and Metamorphic rock.
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The AraçuaÃ-West-Congo Orogen in Brazil: an overview of a confined orogen formed during Gondwanaland assembly
A Pedrosa-Soares.
Precambrian Research (2001)
Kinematic evolution of the Araçuaí-West Congo orogen in Brazil and Africa: Nutcracker tectonics during the Neoproterozoic assembly of Gondwana
Fernando F. Alkmim;Stephen Marshak;Antônio Carlos Pedrosa-Soares;Guilherme Gravina Peres.
Precambrian Research (2006)
Similarities and differences between the Brazilian and African counterparts of the Neoproterozoic Araçuaí-West Congo orogen
A. C. Pedrosa-Soares;F. F. Alkmim;L. Tack;C. M. Noce.
Geological Society, London, Special Publications (2008)
Late Neoproterozoic–Cambrian granitic magmatism in the Araçuaí orogen (Brazil), the Eastern Brazilian Pegmatite Province and related mineral resources
A. C. Pedrosa-Soares;Cristina P. De Campos;Carlos Noce;Luiz Carlos Silva.
Geological Society, London, Special Publications (2011)
Neoproterozoic oceanic remnants in eastern Brazil: Further evidence and refutation of an exclusively ensialic evolution for the Araçuaí–West Congo orogen
Antônio Carlos Pedrosa-Soares;Philippe Vidal;Othon Henry Leonardos;Benjamin Bley de Brito Neves.
Geology (1998)
Evolution of polycyclic basement complexes in the Araçuaí Orogen, based on U–Pb SHRIMP data: Implications for Brazil–Africa links in Paleoproterozoic time
Carlos M. Noce;Antônio Carlos Pedrosa-Soares;Luiz Carlos da Silva;Richard Armstrong.
Precambrian Research (2007)
Orógeno Araçuaí : síntese do conhecimento 30 anos após Almeida 1977.
Antônio Carlos Pedrosa-Soares;Carlos Maurício Noce;Fernando Flecha de Alkmim;Luiz Carlos da Silva.
Revista Geonomos (2013)
Sobre a evolução tectônica do orógeno Araçuaí-Congo ocidental.
Fernando Flecha Alkmim;Antônio Carlos Pedrosa-Soares;Carlos Maurício Noce;Simone Cerqueira Pereira Cruz.
Revista Geonomos (2013)
Toward a new tectonic model for the Late Proterozoic Araçuaí (SE Brazil)-West Congolian (SW Africa) Belt
A.C Pedrosa-Soares;C.M Noce;Ph Vidal;R.L.B.P Monteiro.
Journal of South American Earth Sciences (1992)
Tectono-sedimentary evolution of sedimentary basins from Late Paleoproterozoic to Late Neoproterozoic in the São Francisco craton and Araçuaı́ fold belt, eastern Brazil
M.A Martins-Neto;A.C Pedrosa-Soares;S.A.A Lima.
Sedimentary Geology (2001)
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