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  • 1
    Keywords: basin research ; cratonic basin ; Parnaíba Basin ; Brazil
    Description / Table of Contents: Cratonic basin formation: a case study of the Parnaíba Basin of Brazil / M. C. Daly, R. A. Fuck, J. Julià, D. I. M. Macdonald and A. B. Watts / Geological Society, London, Special Publications, 472, 1-15, 14 September 2018, https://doi.org/10.1144/SP472.20 --- Cratonic basins --- Cratonic basins with reference to the Michigan basin / Norman H. Sleep / Geological Society, London, Special Publications, 472, 17-35, 6 February 2018, https://doi.org/10.1144/SP472.1 --- Lithospheric heating by crustal thickening: a possible origin of the Parnaíba Basin / D. McKenzie and V. Rodríguez Tribaldos / Geological Society, London, Special Publications, 472, 37-44, 19 February 2018, https://doi.org/10.1144/SP472.5 --- A comparative study of the Parnaíba, Michigan and Congo cratonic basins / A. B. Watts, B. Tozer, M. C. Daly and J. Smith / Geological Society, London, Special Publications, 472, 45-66, 22 February 2018, https://doi.org/10.1144/SP472.6 --- The Parnaíba cratonic basin: lithospheric and crustal structure --- Structure of the crust and upper mantle beneath the Parnaíba Basin, Brazil, from wide-angle reflection–refraction data / José E. P. Soares, Randell Stephenson, Reinhardt A. Fuck, Marcus V. A. G. de Lima, Vitto C. M. de Araújo, Flávio T. Lima, Fábio A. S. Rocha and Cíntia R. da Trindade / Geological Society, London, Special Publications, 472, 67-82, 13 April 2018, https://doi.org/10.1144/SP472.9 --- Deep crustal architecture of the Parnaíba basin of NE Brazil from receiver function analysis: implications for basin subsidence / Diogo L. O. Coelho, Jordi Julià, Verónica Rodríguez-Tribaldos and Nicholas White / Geological Society, London, Special Publications, 472, 83-100, 16 May 2018, https://doi.org/10.1144/SP472.8 --- Reprocessing and interpretation of deep structures in a regional transect of the Parnaíba Basin, Brazil / Rafael R. Manenti, Wilker E. Souza and Milton J. Porsani / Geological Society, London, Special Publications, 472, 101-107, 12 June 2018, https://doi.org/10.1144/SP472.17 --- Electrical conductivity structure across the Parnaíba Basin, NE Brazil / F. F. Solon, S. L. Fontes and E. F. La Terra / Geological Society, London, Special Publications, 472, 109-126, 13 July 2018, https://doi.org/10.1144/SP472.19 --- The pre-Silurian Riachão basin: a new perspective on the basement of the Parnaíba basin, NE Brazil / Amanda Porto, Michael C. Daly, Emanuele La Terra and Sergio Fontes / Geological Society, London, Special Publications, 472, 127-145, 19 February 2018, https://doi.org/10.1144/SP472.2 --- Implications of preliminary subsidence analyses for the Parnaíba cratonic basin / Verónica Rodríguez Tribaldos and Nicky White / Geological Society, London, Special Publications, 472, 147-156, 6 February 2018, https://doi.org/10.1144/SP472.3 --- The Parnaíba cratonic basin: stratigraphic and sedimentological evolution --- Evolution of a cratonic basin: insights from the stratal architecture and provenance history of the Parnaíba Basin / L. A. Menzies, A. Carter and David I. M. MacDonald / Geological Society, London, Special Publications, 472, 157-179, 6 August 2018, https://doi.org/10.1144/SP472.18 --- Provenance of sandstones in the Parnaíba Basin through detrital zircon geochronology / M. H. B. M. Hollanda, A. M. Góes and F. A. Negri / Geological Society, London, Special Publications, 472, 181-197, 12 July 2018, https://doi.org/10.1144/SP472.16 --- Palaeogeographical and palaeoclimatic evolution of the intracratonic Parnaíba Basin, NE Brazil using GPlates plate tectonic reconstructions and chemostratigraphic tools / Marwan M. Jaju, Haydon P. Mort, Fadi H. Nader, Mário L. Filho and David I. M. Macdonald / Geological Society, London, Special Publications, 472, 199-222, 6 June 2018, https://doi.org/10.1144/SP472.12 --- Re-evaluation of the Permian macrofossils from the Parnaíba Basin: biostratigraphic, palaeoenvironmental and palaeogeographical implications / Roberto Iannuzzi, Rodrigo Neregato, Juan C. Cisneros, Kenneth D. Angielczyk, Ronny Rößler, Rosemarie Rohn, Claudia Marsicano, Jörg Fröbisch, Thomas Fairchild, Roger M. H. Smith, Francine Kurzawe, Martha Richter, Max C. Langer, Tatiane M. V. Tavares, Christian F. Kammerer, Domingas M. Conceição, Jason D. Pardo and Guilherme A. Roesler / Geological Society, London, Special Publications, 472, 223-249, 2 July 2018, https://doi.org/10.1144/SP472.14 --- The Parnaíba cratonic basin: magmatic history --- Geochemical and temporal provinciality of the magmatism of the eastern Parnaíba Basin, NE Brazil / Monica Heilbron, Eliane Guedes, Miguel Mane, Claudio de Morisson Valeriano, Miguel Tupinambá, Júlio Almeida, Luiz Guilherme do Eirado Silva, Beatriz Paschoal Duarte, Jorge Carlos Dela Favera and Adriano Viana / Geological Society, London, Special Publications, 472, 251-278, 5 June 2018, https://doi.org/10.1144/SP472.11 --- Petrology of Jurassic and Cretaceous basaltic formations from the Parnaíba Basin, NE Brazil: correlations and associations with large igneous provinces / Alisson L. Oliveira, Márcio M. Pimentel, Reinhardt A. Fuck and Diógenes C. Oliveira / Geological Society, London, Special Publications, 472, 279-308, 6 August 2018, https://doi.org/10.1144/SP472.21 --- Role of basaltic magmatism within the Parnaíba cratonic basin, NE Brazil / Marthe Klöcking, Nicky White and John MacLennan / Geological Society, London, Special Publications, 472, 309-319, 23 March 2018, https://doi.org/10.1144/SP472.4 --- Phanerozoic magmatism in the Parnaíba Basin: characterization of igneous bodies (well logs and 2D seismic sections), geometry, distribution and sill emplacement patterns / I. Trosdtorf, J. M. Morais Neto, S. F. Santos, C. V. Portela Filho, T. A. Dall Oglio, A. C. M. Galves and A. M. Silva / Geological Society, London, Special Publications, 472, 321-340, 16 May 2018, https://doi.org/10.1144/SP472.10 --- The Parnaíba cratonic basin: resource system --- Atypical igneous-sedimentary petroleum systems of the Parnaíba Basin, Brazil: seismic, well logs and cores / Frederico S. de Miranda, Ana Luiza Vettorazzi, Paulo R. da Cruz Cunha, Fernando B. Aragão, Diogo Michelon, João Luiz Caldeira, Ernani Porsche, Celso Martins, Roberto B. Ribeiro, Alexandre F. Vilela, José R. Corrêa, Lilian S. Silveira and Kátia Andreola / Geological Society, London, Special Publications, 472, 341-360, 12 July 2018, https://doi.org/10.1144/SP472.15 --- New insights into the Parnaíba Basin: results of investments by the Brazilian National Petroleum Agency / Marina Abelha, Eliane Petersohn, Gabriel Bastos and Daniel Araújo / Geological Society, London, Special Publications, 472, 361-366, 5 July 2018, https://doi.org/10.1144/SP472.13
    Pages: Online-Ressource (VIII, 372 Seiten) , Illustrationen, Diagramme
    ISBN: 9781786203960
    Language: English
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    International journal of earth sciences 71 (1982), S. 291-317 
    ISSN: 1437-3262
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Description / Table of Contents: Abstract The following main units have been recognized as Archaean basement rocks in central Brazil: a) High-grade granite-gneiss terrain composed predominantly by granodioritic and tonalitic gneisses; these rocks are cut by amphibolite dykes and present several nucleii locally surrounded by an array of Archaean greenstone belts, b) Greenstone belts presenting basal komatiitic ultramafic-mafic lavas with abundant spinifex textures, followed by basalts and chemical sediments such as cherts, limestones and graphitic pelites, that are often interbedded with acid and intermediate volcanics; metamorphism is within greenschist facies. Granulite mobile belt, including the granulitized mafic-ultramafic complexes of Barro Alto, Niquelândia and Brava. The Lower Proterozoic is represented by: a) metasedimentary sequences overlying the granite-greenstone terrains, with several tin bearing granite intrusions. b) Gabbro-anorthosite layered plutons and their associated mafic volcanics which are followed by acid and intermediate volcanics and ocean floor sediments. c) Mafic-ultramafic layered intrusions in the granulite terrain.
    Abstract: Resumo As seguintes unidades geológicas principais foram reconhecidas no embasamento da região central do Brasil: a) Terrenos granito-gnáissicos constituídos dominantemente por gnaisses de composição granodiorítica e tonalítica cortados por diques de anfibolito e mostrando vários núcleos graníticos localmente envolvidos por seqüências vulcano-sedimentares do tipo greenstone belt. b) Cinturões arqueanos de rochas verdes apresentando na base lavas komatiíticas com abundantes texturas tipo spinifex, seguidas de basaltos almofadados e de sedimentos químicos tais como chert, calcário e pelitos grafitosos, frequentemente intercalados com vulcânicas intermediárias e ácidas; o metamorfismo é de facies xisto verde. c) Cinturão móvel granulítico incluindo os complexos granulitizados de Barro Alto, Niquelândia e Cana Brava. Proterozóico Inferior é representado por: a) Seqüências sedimentares sobrepostas aos terrenos granito-greenstone, localmente intrudidas por granitos estaniferos; b) Plutões gabro-anortosíticos acamadados; c) Intrusões máfico-ultramáficas alojadas nos terrenos granulíticos. --Краткое содержание В центральной Бразил ии различают следующ ие основные единицы архейских отложений: а) высокоме таморфную гранито-гн ейсовую область с преимущественно гра нодиоритными и тонал итными гнейсами; эти породы пронизаны амфиболит ными жилами и образую т отдельные ядра, окруженные зонами архейского зе ленокаменного пояса, б) Зеленокаменный пояс, представляющий базальные коматиити ческие ультрамафиче ские до мафических лавы с частым проявле нием „спинофексных“ строений. За этими следуют базальты и химически е седименты, как кремн истый сланец, известняки и графитные пелиты, в ко торых часто встречаю т, как включения, кислые и средние вулканиты. Ме таморфизм отмечен в ф ации зеленого сланца; в) под вижный гранулитовый пояс, ко торый включает гранулитизированны е мафическо-ультрама фические комплексы Barro Alto, Niguelandia и Сапа Brava. В нижнем протерозое у становлено присутст вие следующих стратигра фических единиц: а) свиты метасе диментов, перекрытых гранито-зеленокамен ными сериями, и вмещающими некоторые интрузии г ранита, содержащие сурьму; б) прослои габб ро-анортозит-плутоно в с относящимися к ним ма фическими вулканитами, за котор ыми следуют кислые и с редние вулканиты и морски седименты; в) ма фическо-ультрамафич еские интрузии внутри гран улитовой фации.
    Notes: Zusammenfassung Im zentralen Brasilien wurden folgende Haupteinheiten als Archaischer Sockel erkannt: a) hochmetamorphes Granit-Gneis-Gebiet mit vorwiegend granodioritischen und tonalitischen Gneisen; diese Gesteine werden von amphibolitischen Gängen durchschlagen. Sie bilden einzelne Kerne, die von Zonen Archaischer Grünsteingürtel umgeben werden. b) Grünsteingürtel, die basale komatiitische ultramafitische bis mafischen Laven representieren mit häufig auftretenden “Spinifex”-Gefügen. Diesen folgen Basalte und chemische Sedimente wie Kieselschiefer, Kalke und graphitische Pelite, in die häufig saure und intermediäre Vulkanite eingeschaltet sind. Die Metamorphose liegt in der Grünschiefer-Fazies. c) Mobiler Granulit-Gürtel, der die granulitisierten mafisch-ultramafischen Komplexe von Barro Alto, Niquelândia und Cana Brava einschließt. Das untere Proterozoikum wird durch folgende Einheiten vertreten: a) Metasedimentfolgen, die die Granit-Grünstein-Serien überlagern und die einige zinnführende GranitIntrusionen aufweisen. b) Lagige Gabbro-Anorthosit-Plutone mit dazugehörenden mafischen Vulkaniten, die von sauren und intermediären Vulkaniten und ozeanischen Sedimenten gefolgt werden. c) Mafisch-ultramafische Intrusionen innerhalb des Granulit-Gebietes.
    Type of Medium: Electronic Resource
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  • 3
    Publication Date: 2009-09-08
    Description: The Palaeoproterozoic era was the most important stage of crustal accretion in the South American Platform, being responsible for the development of several magmatic arcs, which represent approximately 35% of the present-day continental crust. The recently mapped Campinorte volcano-sedimentary sequence and associated plutonic rocks represent this Palaeoproterozoic history in the northern Brasilia Belt, central Brazil. The sequence consists of metapsammites and metapelites, with interbedded lenses of gondites and metacherts, as well as rhyolite and pyroclastic deposits. Tonalite, granodiorite and granite crystallized between c. 2.18 and 2.16 Ga, as indicated by U-Pb zircon analyses. Sm-Nd TDM model ages range between c. 2.1 and 2.7 Ga, with{varepsilon} Nd values ranging from -2.14 to +3.36, indicating the dominantly juvenile nature of the original magmas. A LA-ICPMS provenance study of zircon grains from a quartzite sample reveals a single sediment source with Palaeoproterozoic age. The data presented here provide new information on the Palaeoproterozoic juvenile crust of central Brazil and suggest correlation with other Palaeoproterozoic provinces, especially the Birimian Belt in West African Craton and those of the Guiana Shield, thus contributing to reconstruction of the Columbia supercontinent.
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  • 4
    Publication Date: 2006-12-01
    Print ISSN: 0148-0227
    Electronic ISSN: 2156-2202
    Topics: Geosciences
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  • 5
    Publication Date: 2020-05-12
    Electronic ISSN: 2045-2322
    Topics: Natural Sciences in General
    Published by Springer Nature
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  • 7
    Publication Date: 2020-10-24
    Print ISSN: 0954-4879
    Electronic ISSN: 1365-3121
    Topics: Geosciences
    Published by Wiley
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  • 8
    Publication Date: 2020-04-01
    Print ISSN: 0301-9268
    Electronic ISSN: 1872-7433
    Topics: Geosciences
    Published by Elsevier
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  • 9
    Publication Date: 2020-12-01
    Print ISSN: 0895-9811
    Electronic ISSN: 1873-0647
    Topics: Geosciences
    Published by Elsevier
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  • 10
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