The structural framework of the north-central Guiana Shield: a fossil fold-and-thrust belt in northeastern Roraima state, Brazil

Página do item simplificado
dc.creatorTulio Mendes
dc.creatorAntonio Oliveira
dc.creatorMarcelo Almeida
dc.creatorFabrício Caxito
dc.creatorTiago Amâncio Novo
dc.date.accessioned2023-10-23T21:08:08Z
dc.date.accessioned2025-09-08T23:38:15Z
dc.date.available2023-10-23T21:08:08Z
dc.date.issued2022-04-29
dc.format.mimetypepdf
dc.identifier.doihttps://doi.org/10.29396/jgsb.2022.v5.n1.2
dc.identifier.issn2595-1939
dc.identifier.urihttps://hdl.handle.net/1843/59860
dc.languageeng
dc.publisherUniversidade Federal de Minas Gerais
dc.relation.ispartofJournal of the Geological Survey of Brazil
dc.rightsAcesso Aberto
dc.subjectTectonica de placas
dc.subjectDesenvolvimento regional - Roraima
dc.subjectFractais
dc.subject.otherNortheastern Roraima
dc.subject.otherMulti-scale structural approach
dc.subject.otherFractal
dc.subject.otherGeometric relations
dc.subject.otherTectonics
dc.titleThe structural framework of the north-central Guiana Shield: a fossil fold-and-thrust belt in northeastern Roraima state, Brazil
dc.typeArtigo de periódico
local.citation.epage19
local.citation.issue1
local.citation.spage1
local.citation.volume5
local.description.resumoThe northeastern Roraima state (Brazil), located in the north-central portion of Guiana Shield, shows shallow-granitoids and associated volcanic rocks of the Orocaima Igneous Belt (2.00-1.96 Ga) overlaid by the Arai Formation sedimentary succession (1.96-1.87 Ga). Previous authors suggested a compressional event affecting the region. Meanwhile, recent papers interpreted that transpressional deformation, related to a distal effect of a Late Mesoproterozoic tectonics (K’Mudku Event), reactivated some basement structures and generated drag folds in the supracrustal successions. This paper presents a multi-scale approach to the best-exposed sector of this geological framework, gathering and analyzing new data from the regional photointerpretation to the thin section scales. The structural data reveal the fractal character and the rheological control on the E-W- and ESE-WNW-trending compressional structures. The southern domain presents sub-vertical shear zones with down-dip to oblique lineation, which are related to the uplift of the shallow-granitoids in relation to the coeval volcanic successions. The central domain, where the volcanic succession crops out, exhibits ubiquitous E-W- to ESE-WNWtrending sub-vertical foliation parallel to the axial plane of the folds. The southern border of the northern domain (Arai Formation) shows spaced cleavage and gentle folds, besides sub-horizontal thrust faults. The structures reveal a fold-and-thrust belt that presents a transition from thick- to thin-skinned tectonics with mass transport to the north. These geometric relations do not match with the K’Mudku lineaments, usually following a NE-SW direction in the north-central Guiana Shield. However, the southward Middle Orosirian structural framework (Uatumã-Anauá Domain) shows similar geometric relations with nearly E-W-trending lineaments and parallel sub-vertical foliation.
local.identifier.orcidhttps://orcid.org/0000-0002-3457-4390
local.identifier.orcidhttps://orcid.org/0000-0002-7874-8444
local.identifier.orcidhttps://orcid.org/0000-0002-7727-091X
local.identifier.orcidhttps://orcid.org/0000-0002-0335-3667
local.identifier.orcidhttps://orcid.org/0000-0002-1999-862X
local.publisher.countryBrasil
local.publisher.departmentIGC - DEPARTAMENTO DE GEOLOGIA
local.publisher.initialsUFMG
local.url.externahttps://jgsb.sgb.gov.br/index.php/journal/article/view/165

Arquivos

Pacote original

Agora exibindo 1 - 1 de 1
Imagem de Miniatura
Nome:
The structural framework of the north-central Guiana Shield_ a fossil fold-and-thrust belt in northeastern Roraima state, Brazil.pdf
Tamanho:
1.95 MB
Formato:
Adobe Portable Document Format
Baixar

Licença do pacote

Agora exibindo 1 - 1 de 1
Imagem de Miniatura
Nome:
License.txt
Tamanho:
1.99 KB
Formato:
Plain Text
Descrição:
Baixar

Coleções

Artigo de Periódico

Logo UFMG