GEOCHEMICAL SIGNATURE OF THE BRASILIANOAGE PLUTONISM IN THE SERIDÓ BELT, NORTHEASTERN BORBOREMA PROVINCE (NE BRAZIL)

dc.contributoren-US
dc.contributorpt-BR
dc.creatorNASCIMENTO, MARCOS ANTONIO LEITE DO
dc.creatorANTUNES, ALEX FRANCISCO
dc.creatorGALINDO, ANTONIO CARLOS
dc.creatorJARDIM DE SÁ, EMANUEL FERRAZ
dc.creatorSOUZA, ZORANO SÉRGIO DE
dc.date2017-04-13
dc.date.accessioned2022-12-15T20:14:46Z
dc.date.available2022-12-15T20:14:46Z
dc.identifierhttps://ppegeo.igc.usp.br/index.php/rbg/article/view/10966
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/5360338
dc.descriptionThe Seridó Belt (Borborema Province, NE Brazil) displays a strong imprint of the late Neoproterozoic Brasiliano orogenic cycle. The most important megascopic structures in the Seridó Belt are strike-slip shear zones, coeval with the emplacement of several granitoid bodies. The paper is based on 217 chemical analyses of the granitoid plutons grouped into five different geochemical suites (Shos - Shoshonitic, PKCAlk - Porphyritic K-Calc-Alkaline, EqKCAlk - Equigranular K-Calc-Alkaline, Alk - Alkaline and ChAlk - Charnockitic Alkaline). They are distinguished by petrographic and textural features, as well as Harker’s and geochemical discriminant diagrams. The Shosis easily distinguished from the others by its low silica content, while the Alk and ChAlk suites have high alkali contents. The PKCAlk and EqKCAlk show similar geochemical behaviour; but they can be separated mainly by petrographic and textural aspects. Field relationships and geochemical affinities suggested that the Shos, PKCAlk, EqKCAlk and Alk are approximately coeval, syntectonic plutons, whereas the ChAlk is interpreted as lateto post-tectonic as regards to the Brasiliano orogeny.en-US
dc.descriptionThe Seridó Belt (Borborema Province, NE Brazil) displays a strong imprint of the late Neoproterozoic Brasiliano orogenic cycle. The most important megascopic structures in the Seridó Belt are strike-slip shear zones, coeval with the emplacement of several granitoid bodies. The paper is based on 217 chemical analyses of the granitoid plutons grouped into five different geochemical suites (Shos - Shoshonitic, PKCAlk - Porphyritic K-Calc-Alkaline, EqKCAlk - Equigranular K-Calc-Alkaline, Alk - Alkaline and ChAlk - Charnockitic Alkaline). They are distinguished by petrographic and textural features, as well as Harker’s and geochemical discriminant diagrams. The Shosis easily distinguished from the others by its low silica content, while the Alk and ChAlk suites have high alkali contents. The PKCAlk and EqKCAlk show similar geochemical behaviour; but they can be separated mainly by petrographic and textural aspects. Field relationships and geochemical affinities suggested that the Shos, PKCAlk, EqKCAlk and Alk are approximately coeval, syntectonic plutons, whereas the ChAlk is interpreted as lateto post-tectonic as regards to the Brasiliano orogeny.pt-BR
dc.formatapplication/pdf
dc.languageeng
dc.publisherSociedade Brasileira de Geologiapt-BR
dc.relationhttps://ppegeo.igc.usp.br/index.php/rbg/article/view/10966/10420
dc.rightsDireitos autorais 2017 Revista Brasileira de Geociênciaspt-BR
dc.sourceRevista Brasileira de Geociências; v. 30, n. 1 (2000); 161-164en-US
dc.sourceRevista Brasileira de Geociências; v. 30, n. 1 (2000); 161-164es-ES
dc.sourceRevista Brasileira de Geociências; v. 30, n. 1 (2000); 161-164pt-BR
dc.source0375-7536
dc.subjectSeridó Belt; Brasiliano orogeny; Plutonism; Geochemistry; Discriminant diagrams.en-US
dc.subjectSeridó Belt; Brasiliano orogeny; Plutonism; Geochemistry; Discriminant diagrams.pt-BR
dc.titleGEOCHEMICAL SIGNATURE OF THE BRASILIANOAGE PLUTONISM IN THE SERIDÓ BELT, NORTHEASTERN BORBOREMA PROVINCE (NE BRAZIL)en-US
dc.titleGEOCHEMICAL SIGNATURE OF THE BRASILIANOAGE PLUTONISM IN THE SERIDÓ BELT, NORTHEASTERN BORBOREMA PROVINCE (NE BRAZIL)pt-BR
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion
dc.typept-BR


Este ítem pertenece a la siguiente institución