| 1. Identificação | |
| Tipo de Referência | Artigo em Revista Científica (Journal Article) |
| Site | plutao.sid.inpe.br |
| Código do Detentor | isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S |
| Identificador | J8LNKAN8RW/39RQF8U |
| Repositório | dpi.inpe.br/plutao/2011/06.11.03.44.32 (acesso restrito) |
| Última Atualização | 2011:07.25.14.35.20 (UTC) administrator |
| Repositório de Metadados | dpi.inpe.br/plutao/2011/06.11.03.44.33 |
| Última Atualização dos Metadados | 2018:06.05.00.01.20 (UTC) administrator |
| Chave Secundária | INPE--PRE/ |
| DOI | 10.1016/j.precamres.2010.12.003 |
| ISSN | 0301-9268 |
| Rótulo | lattes: 7089299825777600 4 BolognaPadiVitoPádu:2011:SiCoCo |
| Chave de Citação | BolognaPadiVitoPádu:2011:SiCoCo |
| Título | Signatures of continental collisions and magmatic activity in central Brazil as indicated by a magnetotelluric profile across distinct tectonic provinces  |
| Projeto | FAPESP 95/0687-4 00/00806-5 01/02848-0 CNPq 142617/97-0 350683/94-8 351398/94-5 |
| Ano | 2011 |
| Mês | Feb. |
| Data de Acesso | 26 maio 2024 |
| Tipo Secundário | PRE PI |
| Número de Arquivos | 1 |
| Tamanho | 1559 KiB |
| 2. Contextualização | |
| Autor | 1 Bologna, Maurício S. 2 Padilha, Antonio L. 3 Vitorello, Ícaro 4 Pádua, Marcelo Banik de |
| Identificador de Curriculo | 1 2 3 8JMKD3MGP5W/3C9JHD6 4 8JMKD3MGP5W/3C9JHNR |
| Grupo | 1 DGE-CEA-INPE-MCT-BR 2 DGE-CEA-INPE-MCT-BR 3 DGE-CEA-INPE-MCT-BR 4 DGE-CEA-INPE-MCT-BR |
| Afiliação | 1 Instituto Nacional de Pesquisas Espaciais (INPE) 2 Instituto Nacional de Pesquisas Espaciais (INPE) 3 Instituto Nacional de Pesquisas Espaciais (INPE) 4 Instituto Nacional de Pesquisas Espaciais (INPE) |
| Endereço de e-Mail do Autor | 1 2 padilha@dge.inpe.br 3 4 banik@dge.inpe.br |
| Endereço de e-Mail | banik@dge.inpe.br |
| Revista | Precambrian Research |
| Volume | 185 |
| Número | 1-2 |
| Páginas | 55-64 |
| Nota Secundária | A2_ENGENHARIAS_II A1_GEOCIÊNCIAS A1_INTERDISCIPLINAR |
| Histórico (UTC) | 2011-06-11 17:43:46 :: lattes -> marciana :: 2011 2011-11-10 12:59:55 :: marciana -> administrator :: 2011 2018-06-05 00:01:20 :: administrator -> tereza@sid.inpe.br :: 2011 |
| 3. Conteúdo e estrutura | |
| É a matriz ou uma cópia? | é a matriz |
| Estágio do Conteúdo | concluido |
| Transferível | 1 |
| Tipo do Conteúdo | External Contribution |
| Tipo de Versão | publisher |
| Palavras-Chave | Upper mantle Central Brazil Magnetotellurics Seismic low velocity anomaly Refertilization SAO-FRANCISCO CRATON ELECTRICAL-CONDUCTIVITY BRASILIA BELT HEAT-FLOW SE BRAZIL MANTLE ANISOTROPY ROCKS INVERSION CRUSTAL |
| Resumo | Broadband and long-period magnetotelluric soundings were collected along a 560 km E-W profile in a region of central Brazil subjected to Neoproterozoic collision tectonics and Archean to Cretaceous magmatic events. The profile crosses the northeastern portion of Phanerozoic sediments and volcanics of the Parana basin, the southern extension of the Neoproterozoic metasedimentary rocks of the Brasilia belt, locally pervaded by Cretaceous alkaline magmas of the Alto Paranaiba igneous province (APIP), and Neoproterozoic sedimentary cover and exposed Archean basement of the southern Sao Francisco craton. 2D conductivity structures derived by joint inversions of the TE and TM polarization modes and a separate inversion of the tipper components show signatures of the past tectonomagmatic events that affected the area. A gravity-defined suture zone beneath the Parana basin is detected in the models as a subvertical conductor extending from crustal to upper mantle depths, which strengthen the interpretation of a Neoproterozoic collision of the Sao Francisco craton and a continental block beneath the sedimentary basin. Deep underthrusting of organic graphite-bearing metasedimentary rocks composing a fossil suture zone is proposed to explain such increase in electrical conductivity. A similar conductivity signature beneath the sedimentary covered region of the Sao Francisco craton can be tentatively interpreted as another similar cryptic suture zone. Other isolated high-conductivity anomalies at midcrustal depths below the Parana and APIP provinces are interpreted as fossil residues representing precipitated graphite and sulfide derived from percolating volatiles during the emplacement of Cretaceous mafic-ultramafic volcanics. A very high conductivity wedge into the lower lithosphere is highlighted in the deep mantle beneath the APIP volcanic complex, coincident with a zone of low velocity defined by seismic tomography. Geochemical evidence indicates that the alkaline magmatism stemmed from a metasomatized upper mantle at only slightly raised temperatures. Thus, interconnected carbonatite melts of low melting point and graphite in the lithospheric mantle are the most likely candidates to explain this high conductivity. The seismic and conductivity anomalies are probably triggered by the same source mechanisms (incipient melting) because they are plausibly related to the same magmatic process. Conductivity anomalies at crustal and mantle depths in the southern segment of the Sao Francisco craton suggest that its lithosphere was significantly affected by the several tectonomagmatic episodes it has experienced throughout its geological history. Consequently, the enhanced conductivity in the lower crust can be genetically related to upwelling volatile-rich intrusions whereas upper mantle high conductivity can be related to refertilization by infiltrations of low-degree carbonatitic melts from deeper-sourced metasomatic processes. |
| Área | CEA |
| Arranjo | urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDGE > Signatures of continental... |
| Conteúdo da Pasta doc | acessar |
| Conteúdo da Pasta source | não têm arquivos |
| Conteúdo da Pasta agreement | não têm arquivos |
| 4. Condições de acesso e uso | |
| Idioma | en |
| Arquivo Alvo | sdarticle-4.pdf |
| Grupo de Usuários | administrator lattes marciana |
| Visibilidade | shown |
| Política de Arquivamento | denypublisher denyfinaldraft24 |
| Permissão de Leitura | deny from all and allow from 150.163 |
| Permissão de Atualização | não transferida |
| 5. Fontes relacionadas | |
| Unidades Imediatamente Superiores | 8JMKD3MGPCW/3EU29DP |
| Divulgação | WEBSCI; PORTALCAPES; COMPENDEX. |
| Acervo Hospedeiro | dpi.inpe.br/plutao@80/2008/08.19.15.01 |
| 6. Notas | |
| Campos Vazios | alternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn lineage mark mirrorrepository nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress readergroup rightsholder schedulinginformation secondarydate session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url |
| 7. Controle da descrição | |
| e-Mail (login) | tereza@sid.inpe.br |
| atualizar | |