[PDF] Top 20 Braz. J. Geol. vol.46 número2

... he most conident paleo ice-low indicators in the Paraná Basin are streamlined landforms, such as whale- backs and moutonnées , striated pavements on rigid beds, and subglacial soft-se[r] ... See full document

... he collision between continental masses during the formation of supercontinents triggers the closing of oceans in subduction zones and the generation of magmatic arcs with intense production of granitic magmatism ... See full document

... Teixeira S.G. & Soares E.A.A. 2011. Uso de imagens multi-sensores na identiicação de paleocanais na planície aluvial do Rio Solimões, Amazônia Ocidental. In: XIII Congresso da Associação Brasileira de Estudos do ... See full document

... But, from the end of the Oligocene to the beginning of the Late Miocene, both the Purus Arch and sedimentary basins were the focus of sub- sidence and sedimentation, with the depositio[r] ... See full document

... Li Z.X., Bogdanova S.V., Collins A.S., Davidson A., De Waele B., Ernst R.E., Fitzsimons I.C.W., Fuck R.A., Gladkochub D.P., Jacobs J., Karlstrom K.E., Lu S., Natapov L.M., Pease V., Pisarevsky S.A., Thrane K., ... See full document

... A irst model that takes into consideration the four evidential layers (ASA, h/K ratio, elevation and slope) for the whole study area permits inference on possibilities for supergene n[r] ... See full document

... Faria D.A., Ruiz A.S., Matos J.B., Sousa M.Z.A., Lima G.A., Moacir J.B.M. 2014. Geology geochemistry and geochronology (U-Pb) of the Rio Fortuna Gneiss – Serra do Baú Intrusive Suite – Paraguá Terrane – SW Amazonian ... See full document

... Pedrosa-Soares A.C., Campos C.P., Noce C., Silva L.C., Novo T., Roncato J., Medeiros S., Castañeda C., Queiroga G., Dantas E., Dussin I., Alkmim F.F. 2011a. Late Neoproterozoic-Cambrian granitic magmatism in the ... See full document

... Santos M.E.C.M. & Carvalho M.S.S. 2004. Paleontologia das bacias do Parnaíba, Grajaú e São Luís. Programa de Levantamentos Geológicos Básicos do Brasil. CPRM, Serviço Geológico do Brasil/DIEDIG/DEPAT, Rio de Janeiro, ... See full document

... Imagens de biotita-muscovita-quartzo xisto: (A) aspecto macroscópico dos xistos com xistosidade deinida por muscovita e quartzo; (B) textura lepidoblástica marcada po[r] ... See full document

... Mauro Daniel Rodrigues Bruno Instituto Tecnológico de Micropaleontologia – itt Fossil, Universidade do Vale do Rio dos Sinos (UNISINOS), Cidade de São Leopoldo (RS), Brasil. Welcome to [r] ... See full document

... he proposed paleogeographic reconstruction comprises several elongated, shallow, branched gulf-like tongues connecting the Western Tethys with interior (Parnaíba, Araripe, Recôncavo, [r] ... See full document

... It should also be recalled that the Aptian Northeast Brazilian Seaway was not a direct consequence of the con- tinental breakup, being unrelated directly to the South Atlantic opening. he primitive South Atlantic has ... See full document

... he São Sebastião and Marizal formations were the subject of previous studies, which made possible the comparison of Ground Penetrating Radar survey to previous stratigraphic studies i[r] ... See full document

... Fretwell P., Pritchard H.D., Vaughan D.G., Bamber J.L., Barrand N.E., Bell R., Bianchi C., Bingham R.G., Blankenship D.D., Casassa G., Catania G., Callens D., Conway H., Cook A.J., Corr H.F. J., Damaske D., Damm ... See full document

... In order to contribute to the understanding of the man- tle sources involved in PCFB, this study presents the irst Pb isotope data and a review of published major, minor and incompatib[r] ... See full document

... Finally, we would like to thank Professor Umberto Cordani for his eforts in helping create and further develop the Geochronological Research Center at Universidade de São Paulo, and als[r] ... See full document

... Rocks in the area of São Gabriel da Cachoeira and the Içana River, in NW Brazil, are well within the Rio Negro-Juruena province, and very likely have primary ages between 1800 and 150[r] ... See full document

... Figure 4. Photos from the Cabo Frio Tectonic Domain units. (A) 1.97 Ga coarse grained granite with dioritic enclaves, probably coeval and related to magma mingling; (B) Cross-cutting contact between the foliated 1.98 Ga ... See full document

... he greenstone belts successions are made of a basal ultra- maic unit made of komatiites, locally presenting well-pre- served spinifex textures and pillow structures, covered by a metabasalt unit with intercalations of ... See full document