
Roberto Naime, Lauro Valentim Stoll Nardi,
O Granito da Ramada e uma intrusao epizonal, pos-orogenica, associada ao magmatismo alcalino que sucede a orogenese brasiliana. Ele e constituido por sieno e monzogranitos com anfibolio calcico (magnesio homblenda e homblenda feno-edenitica) e biotita, alem de magnetita, ihnenita, titanita, zircao, allanita e fluorita. Sua textura varia de equigranular hipidiomorfica ate porfiritica. Sua composicao quimica nao e tipicamente alcalina, sendo este carater indicado pelas razoes FeO(t)/FeO(t)+MgO superiores ...
Tópico(s): earthquake and tectonic studies
1991 - Sociedade Brasileira de Geologia | Brazilian Journal of Geology

Fernando Flávio Marques de Almeida,
A comparative study of the Precambrian tectonic differentiation of the Guapore Craton in South America, and the Baltic Shield in Europe, demonstrate that the major geologic events are synchronous and correlatables. The Transamazonian and Svecofennian-Karelian cycles are equivalent in age and geologic products, as well as the volcanic phenomena Uatuma and sub-Jotnian, which were both accompanied and followed by anorogenic granites between 1,700 and 1,500 m.y. The subsequent clastic Precambrian covers ...
Tópico(s): Geochemistry and Geologic Mapping
1974 - Sociedade Brasileira de Geologia | Brazilian Journal of Geology

Fernando Flávio Marques de Almeida,
A comparative study of the Precambrian tectonic differentiation of the Guaporé Cráton in South America, and the Baltic Shield in Europe, demonstrate that the major geologic events are synchronous and correlatables. The Transamazonian and Svecofennian-Karelian cycles are equivalent in age and geologic products, as well as the volcanic phenomena Uatumã and sub-Jotnian, which were both accompanied and followed by anorogenic granites between 1,700 and 1,500 m.y. The subsequent clastic Precambrian covers ...
Tópico(s): Planetary Science and Exploration
1974 - Sociedade Brasileira de Geologia | Revista Brasileira de Geociências

ANDRÉ DE BORBA, Anderson José Maraschin, Ana Maria Pimentel Mizusaki,
Significant improvement in the knowledge concerning the Neoproterozoic Maricá Formation of the Sul-riograndense Shield, southern Brazil, was obtained in the latest years. This contribution synthesizes recent data obtained though an integrated analysis of the lowermost unit of the “Camaquã Basin”. Stratigraphic and paleocurrent analyses, petrography, Sr and Nd isotope geology, U-Pb SHRIMP geochronology and Ar-Ar dating were applied to the sedimentary and volcanogenic record of the Maricá Formation ...
Tópico(s): Geochemistry and Elemental Analysis
2007 - | Pesquisas em Geociências

Daniel Triboli Vieira, Edinei Koester, Anelise Losangela Bertotti,
RESUMO: O Granito Chasqueiro aflora como campos de matacões e lajeados, que em planta constituem um corpo alongado segundo N50oE com área de aproximadamente 400 km2, localizado no sul da porção oriental do Escudo Sul-Rio-Grandense. Compreende de monzo a sienogranito, leucocrático de cor cinza-clara e textura porfirítica com megacristais de K-feldspatos em matriz equigranular, hipidiomórfica grossa, composta por quartzo, K-feldspato, plagioclásio, biotita, hornblenda, minerais opacos e acessórios. ...
Tópico(s): earthquake and tectonic studies
2016 - Sociedade Brasileira de Geologia | Brazilian Journal of Geology

Carlos Alberto Spier, César Fonseca Ferreira Filho,
The Vila Nova Project covers an area of 170 km 2 located at the center-southeast of the Amapa State, Brazil. The Project area comprises granite-gneiss terrains, mafic-ultramafic rocks, volcanic-sedimentary association and intrusive granitic and basic intrusive. Upper amphibolite facies metamorphism affected the mafic-ultramafic rocks as well as the volcanic-sedimentary association. Several ore bodies of chromium, gold and iron together with occurrences of diamond and tantalite indicate the anomalous ...
Tópico(s): Geological and Geochemical Analysis
1999 - Sociedade Brasileira de Geologia | Brazilian Journal of Geology

Carlos Alberto Spier, César Fonseca Ferreira Filho,
The Vila Nova Project covers an área of 170 km 2 located at the center-southeast of the Amapa State, Brazil. The Project area comprises granite-gneiss terrains, mafic-ultramafic rocks, volcanic-sedimentary association and intrusive granitic and basic intrusive. Upper amphibolite facies metamorphism affected the mafic-ultramafïc rocks as well as the volcanic-sedimentary association. Several ore bodies of chromium, gold and iron together with occurrences of diamond and tantalite indicate the anomalous ...
Tópico(s): Geological and Geochemical Analysis
1999 - Sociedade Brasileira de Geologia | Revista Brasileira de Geociências

ROBERTO H. NAIME, LAURO V.S. NARDI,
PETROLOGY AND GEOCHEMISTRY.The Ramada Granite is a post-OTogenic, epizonal intrusion, associated to alkaline magmatism which postdates die Brasiliano orogenesis.It is composed of aeno and monzogranites containing calcic-amphibofes (magnesium hornblende and feno-edenitic hornblende) and biotite, besides magnetite, ilmenite, titanite, zircon, allanite, and fluorite.Their textures vary from hypidiomorphic equigranular to porphyritic.As far as chemical composition is concerned they are not typically ...
Tópico(s): Geography and Environmental Studies
1991 - Sociedade Brasileira de Geologia | Revista Brasileira de Geociências

Vinícius Matté, Carlos Augusto Sommer, Evandro Fernandes de Lima, Dejanira Lüderitz Saldanha, Jussara Alves Pinheiro-Sommer, Joaquim Daniel de Liz,
Studies carried out in the Ramada Plateau (Western of the Rio Grande do Sul State, Brazil), have allowed the characterization of a dioritic hipabissal body, which is intrusive in pyroclastic rocks of the Acampamento Velho Formation. This unit consists of volcanic rocks of predominantly silicic composition in association with basic rocks, and it corresponds to the extrusive portion of the sodic alkaline magmatism of the Neoproterozoic age (570-550 Ma), related to postcollisional events of the Brasiliano- ...
Tópico(s): Geochemistry and Geologic Mapping
2012 - Sociedade Brasileira de Geologia | Revista Brasileira de Geociências

Maria do Carmo Pinto Gastal, Francisco José Fonseca Ferreira, Jefferson Ulisses da Cunha, Camila Esmeris, Edinei Koester, María Irene Bartolomeu Raposo, Marcos de Magalhães May Rossetti,
<p>A construção do granito Lavras é analisada mediante integração de dados geológicos, geofísicos e estruturais originais e compilados, em consonância com a evolução do centro vulcano-plutônico. Esse centro engloba o complexo intrusivo Lavras do Sul e a sequência traquiandesítica da Formação Hilário (604 - 590 Ma), ambos formados em posição de antepaís durante o período pós-colisional da Orogênese Dom Feliciano, no oeste do Escudo Sul-riograndense. A análise de estruturas rúpteis e lineamentos ...
Tópico(s): earthquake and tectonic studies
2015 - Sociedade Brasileira de Geologia | Brazilian Journal of Geology

STEPHEN E. HALLINAN, Marta Sílvia Maria Mantovani, WLADIMIR SHUKOWSKY, IRALDO BRAGGION,
New gravity data in southern Brazil are combined with previous data in Brazil and Uruguay, permitting detailed analysis of the basement structure. The Brasiliano cycle tectonic frameworks suggested by previous geological and geophysical studies are tested. Pre-Brasilianp structure (Transamazonian cycle), however, is an importam and hitherto unstated source of lateral density contrast responsible for distinctive gravity discontinuities. Gravity anomalies associated with Mesozoic magmatism are also ...
Tópico(s): Geography and Environmental Studies
1993 - Sociedade Brasileira de Geologia | Revista Brasileira de Geociências

S. Hallinan, Marta Sílvia Maria Mantovani, Wladimir Shukowsky, Iraldo Braggion,
New gravity data in southern Brazil are combined with previous data in Brazil and Uruguay, permitting detailed analysis of the basement structure. The Brasiliano cycle tectonic frameworks suggested by previous geological and geophysical studies are tested. Pre-Brasilianp structure (Transamazonian cycle), however, is an importam and hitherto unstated source of lateral density contrast responsible for distinctive gravity discontinuities. Gravity anomalies associated with Mesozoic magmatism are also ...
Tópico(s): Geophysics and Gravity Measurements
1993 - Sociedade Brasileira de Geologia | Brazilian Journal of Geology

Maria do Carmo Pinto Gastal, Jean Michel Lafon,
The mctaluminous granites with alkaline affinity or tendency occur in lhe west and east portions of the Sul-riograndense Shield. They are separated in three groups. Although ali three might be related to A-type granites, in the wide sense of the term, theirgeochemical and isotopic features reflect differences in the sources or in the generation processes. These granites, in the east, have highly fractionated calc-alkaline nature, with alkaline tendency and are derived from sources enriched in K ...
Tópico(s): earthquake and tectonic studies
1998 - Sociedade Brasileira de Geologia | Brazilian Journal of Geology

Maria do Carmo Pinto Gastal, Jean Michel Lafon,
SUL-RIOGRANDENSE SHIELD: GEOCHEMIST, AND Rb-Sr AND Pb-Pb ISOTOPES The mctaluminous granites with alkaline affinity or tendency occur in lhe west and east portions of the Sul-riograndense Shield.They are separated in three groups.Although ali three might be related to A-type granites, in the wide sense of the term, theirgeochemical and isotopic features reflect differences in the sources or in the generation processes.These granites, in the east, have highly fractionated calc-alkaline nature, with ...
Tópico(s): Geography and Environmental Studies
1998 - Sociedade Brasileira de Geologia | Revista Brasileira de Geociências

Luis Alberto D‘Ávila Fernandes, Rualdo Menegat, Antônio Flávio Uberti Costa, Edinei Koester, Carla Cristine Porcher, Andreia Tommasi, Gustavo Kraemer, Gilberto Emílio Ramgrab, Eduardo Camozzato,
The recognition of three geophysical domains has permitted a re-evaluation of the geotectonic models proposed for the precambrian rocks of the Sul-rio-grandense shield. The eastern, central and western geophysical domains are separated by important gravimetric and aeromagnetic discontinuities and consist of assemblages of rocks with petrogenetic characteristics of specific tectonic environments. The eastern domain includes two neoproterozoic calc-alkaline plutonic sequences, typical of active margin ...
Tópico(s): Geography and Environmental Studies
1995 - Sociedade Brasileira de Geologia | Brazilian Journal of Geology

Luis Alberto D‘Ávila Fernandes, Rualdo Menegat, ANTÓNIO FLÁVIO UBERTI COSTA, Edinei Koester, Carla Cristine Porcher, ANDREIA TOMMASI, GUSTAVO KRAEMER, GILBERTO EMÍLIO RAMGRAB, EDUARDO CAMOZZATO,
RESUMO O reconhecimento de três blocos geofísicos no Escudo Sul-rio-grandense, a partir de técnicas gravimétricas e aeromagnetométricas, permitiu uma reavaliação e teste dos modelos de compartimentação geotectônica propostos a partir do registro geológico para as rochas pré-Cambrianas.Os blocos geofísicos ocidental, central e oriental são separados por importantes descontinuidades gravimétricas e aeromagnetométri-
Tópico(s): Geography and Environmental Studies
1995 - Sociedade Brasileira de Geologia | Revista Brasileira de Geociências

Luis Alberto D‘Ávila Fernandes, Rualdo Menegat, ANTÔNIO FLÁVIO UBERTI COSTA, Edinei Koester, Carla Cristine Porcher, ANDREIA TOMMASI, GUSTAVO KRAEMER, GILBERTO EMÍLIO RAMGRAB, EDUARDO CAMOZZATO,
A reappraisal of the geological basis of a Plate Tectonics model proposed for the tectonic evolution of the Dom Feliciano Belt in the Sul-rio-grandense Shield is presented under the light of a research programme in geology.Folio wing the presentation of a synthesis about the nature and structural characteristics of each geotectonic unit recognised, the main geotectonic models presented for this belt are discussed under the conceptual and substantive point of view.A discussion about the nature and ...
Tópico(s): Geological Modeling and Analysis
1995 - Sociedade Brasileira de Geologia | Revista Brasileira de Geociências

Rodrigo Chaves Ramos, Edinei Koester,
No Rio Grande do Sul são reconhecidas e descritas diversas ocorrências de rochas ultramáficas nas porções central e ocidental do Escudo Sul-rio-grandense. No entanto, para a porção oriental, nenhum trabalho de cunho científico fez referência a esse tipo de litologia até o momento. No presente artigo é apresentado o estudo de uma associação de rochas máficas e ultramáficas metamorfizadas, localizada no extremo sul da por- ção oriental do Escudo, nas proximidades do município de Arroio Grande. Através ...
Tópico(s): Geochemistry and Geologic Mapping
2014 - | Pesquisas em Geociências

Márcio de Souza Soares, Jair Carlos Koppe, João Felipe Coimbra Leite Costa, Sílvia Beatriz Alves Rolim,
... localizadas na Seqüência Campestre do Complexo Bossoroca no Escudo Sul-Rio-Grandense. Nessa região foi realizado um levantamento aerogeofísico, onde mapas gamaespectrométricos (K, U, Th e contagem total) geraram informações sobre a geologia e possíveis alvos para futuras explorações minerais. Baseado ...
Tópico(s): Geophysical and Geoelectrical Methods
2004 - SciELO | Rem Revista Escola de Minas
Jaime Galvis, Alcides Huguett, Primitivo Ruge,
... éólico, terrazas y aluviones recientes. El fracturamiento del Escudo presenta dos direcciones principales que varían de NNE a NW. Las estructuras sedimentarias precámbricas aparecen plegadas y fracturadas, con una orientación general NNW - NW. El resto de las estructuras se caracteriza por su disposición horizontal. En lo referente a Geología Económica, es necesario anotar la ausencia de los dos tipos de yacimientos más importantes en la era precámbrica de todo el mundo, las ta conitas y los sulfuros masivos asociados a cinturones de rocas básicas. Así, el interés que presenta la parte colombiana del Escudo de Guayana, se dirige más hacia los radioactivos ...
Tópico(s): Water Resource Management and Quality
1979 - | Boletín Geológico

Mariana Maturano Dias Martil, Maria de Fátima Bitencourt, Lauro Valentim Stoll Nardi,
... Encruzilhada do Sul, RS, e faz parte do Escudo Sul-rio-grandense (ESRG). Congrega rochas ortometamórficas de composição tonalítica, além de paragnaisses pelíticos e calciossilicáticos. Orto e paragnaisses são intercalados em fatias de 3 a 4m de espessura média e apresentam paragêneses e microestruturas compatíveis com metamorfismo de fácies granulito. A abordagem integrada de geologia de campo, geologia estrutural e petrografia permitiu discutir ...
Tópico(s): Geochemistry and Geologic Mapping
2011 - | Pesquisas em Geociências

Luis Alberto D‘Ávila Fernandes, Rualdo Menegat, Antônio Flávio Uberti Costa, Edinei Koester, Carla Cristine Porcher, Andreia Tommasi, Gustavo Kraemer, Gilberto Emílio Ramgrab, Eduardo Camozzato,
A reappraisal of the geological basis of a Plate Tectonics model proposed for the tectonic evolution of the Dom Feliciano Belt in the Sul-rio-grandense Shield is presented under the light of a research programme in geology. Folio wing the presentation of a synthesis about the nature and structural characteristics of each geotectonic unit recognised, the main geotectonic models presented for this belt are discussed under the conceptual and substantive point of view. A discussion about the nature ...
Tópico(s): Geography and Environmental Studies
1995 - Sociedade Brasileira de Geologia | Brazilian Journal of Geology

Marcelo Esteves Almeida, Moacir José Buenano Macambira,
Regional mapping carried out in the Uatuma-Anaua Domain (UAD), Guyana Shield, southeastern Roraima (Brazil), has showed widespread calc-alkaline granitic to alkaline magmatism and local peraluminous granites. These granitoid rocks are distributed into several magmatic associations with different Paleoproterozoic (1.97-1.89 Ga) ages, structural and geochemical affinities. In this paper, detailed mapping and petrographic studies have distinguished two main subdomains in UAD. In the northern UAD, the ...
Tópico(s): Geography and Environmental Studies
2016 - Sociedade Brasileira de Geologia | Revista Brasileira de Geociências
Paul C. Hackley, Franco Urbani, Alex W. Karlsen, Christopher P. Garrity,
... fueron integrados con el mapa geologico digital del Escudo de Guayana Venezolano, a su vez derivado de hojas en papel a escala 1:500.000. La informacion sobre los tipos de fallas mostrados en el mapa es igual que en las fuentes originales. Los poligonos geologicos fueron atribuidos por edad, litologia y nombre de la unidad siguiendo el Codigo geologico de Venezuela. Se incorporaron revisiones significativas de la geologia de la Cordillera de la Costa a partir ...
Tópico(s): Environmental and Ecological Studies
2006 - United States Department of the Interior | Antarctica A Keystone in a Changing World

No presente trabalho o autor estuda o tipo de tectonismo que afetou o escudo brasileiro após a ultim a revolução orogenetica registrada no dobramento da serie Bambuí (diastrofismo caledonico?) e conclue pela existencia de um so tipo de deformação tectonica no Brasil responsável pela sua historia geologica do devoniano aos tempos atuais, o de caracter epeirogenico. Os fundam entos desta tectonica acham-e em dados estratigraficos, geomorficos, estruturais e fisiograficos, sendo reduzido o numero dos ...
Tópico(s): Geography and Environmental Studies
1951 - | Boletim da Faculdade de Filosofia Ciências e Letras Universidade de São Paulo Geologia
Javier Guerrero, Gustavo Sarmiento, Rosa Esther Narrete,
... Cordillera Central y otra al E en el Escudo de Guyana. Los estratos en el lado W ... las rocas sedimentarias del Precambrico y Paleozoico del Escudo de Guyana. Los ambientes sedimentarios del VSM fueron ...
Tópico(s): Geological and Tectonic Studies in Latin America
2000 - | Geología Colombiana

Carlos Augusto Sommer, Evandro Fernandes de Lima, Lauro Valentim Stoll Nardi,
... Pedrito, RS esta localizado na porcao oeste do Escudo Sul-riograndense. Esta unidade Neoproterozoica e referida geralmente ... assim as ultimas manifestacoes do Ciclo Brasiliano no Escudo Sul-riograndense.
Tópico(s): Geochemistry and Geologic Mapping
1999 - Sociedade Brasileira de Geologia | Brazilian Journal of Geology
This paper contains petrographic and field observations about the lithologic units obsserved in the Caranacoa and Naquen Ranges, situated in Guainia Departament, Colombia. It is postulated a Hypothesis about the gold ocurrences known in those ranges. Such hypothesis proposes a gold precipitation from chemically reducing brines caused by oxygen expelled by anaerobic organisms.
Tópico(s): Geological and Tectonic Studies in Latin America
1993 - | Geología Colombiana
Juan Carlos Carracedo, Hervé Guillou, Eduardo Rodríguez Badiola, Francisco-José Pérez-Torrado, Alejandro Rodríguez-González, Raphaël Paris, Valentín R. Troll, S. Wiesmaier, Audray Delcamp, J. L. Fernández-Turiel,
... típicos de los estadios juveniles de desarrollo en escudo, como los más tardíos, correspondientes a las fases ... formó como una extensión hacia el NE del escudo central de Tenerife, donde aflora debajo del macizo ...
Tópico(s): Geological and Tectonic Studies in Latin America
2009 - Spanish National Research Council | Estudios Geológicos

Lêda Maria Barreto Fraga, Regina Clélia Haddad, Nélson Joaquim Reis,
... de cisalhamento, no norte do Estado de Roraima, Escudo das Guianas, representando um magmatismo tardi- a pos- ... pos-colisional relacionado ao Ciclo Transamazonico, interpretado no Escudo das Guianas como resultante da evolucao de arcos ...
Tópico(s): Geochemistry and Geologic Mapping
1997 - Sociedade Brasileira de Geologia | Brazilian Journal of Geology