| 1. Identificação | |
| Tipo de Referência | Artigo em Revista Científica (Journal Article) |
| Site | mtc-m12.sid.inpe.br |
| Código do Detentor | isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S |
| Identificador | 6qtX3pFwXQZ3ukuKE/CQ74h |
| Repositório | sid.inpe.br/sergio/2004/07.21.12.37 (acesso restrito) |
| Última Atualização | 2015:09.15.12.07.00 (UTC) marciana |
| Repositório de Metadados | sid.inpe.br/sergio/2004/07.21.12.37.38 |
| Última Atualização dos Metadados | 2018:06.05.00.40.51 (UTC) administrator |
| Chave Secundária | INPE-11425-PRE/6857 |
| ISSN | 0101-9082 |
| Chave de Citação | VenezianiSantPara:2004:MoBaDa |
| Título | A Evolução tectono-estratigráfica da província mineral de Carajás: um modelo com base em dados de Sensores Remotos Orbitais (SAR-C RADARSAT-1, TM Landsat -5), Aerogeofísica e Dados de Campo  |
| Projeto | Sensoriamento Remoto Aplicado à Geologia |
| Ano | 2004 |
| Mês | mar. |
| Data de Acesso | 03 maio 2024 |
| Tipo Secundário | PRE PN |
| Número de Arquivos | 2 |
| Tamanho | 11027 KiB |
| 2. Contextualização | |
| Autor | 1 Veneziani, Paulo 2 Santos, Athos Ribeiro dos 3 Paradella, Waldirt Renato |
| Identificador de Curriculo | 1 2 8JMKD3MGP5W/3C9JGKB |
| Grupo | 1 DSR-INPE-MCT-BR 2 DSR-INPE-MCT-BR 3 DSR-INPE-MCT-BR |
| Revista | Geociências |
| Volume | 34 |
| Número | 1 |
| Páginas | 67-78 |
| Histórico (UTC) | 2006-05-18 13:52:30 :: marciana -> administrator :: 2008-06-09 19:22:44 :: administrator -> banon :: 2009-08-04 17:27:25 :: banon -> administrator :: 2014-05-01 11:07:32 :: administrator -> marciana :: 2004 2015-09-15 12:07:01 :: marciana -> administrator :: 2004 2018-06-05 00:40:51 :: administrator -> marciana :: 2004 |
| 3. Conteúdo e estrutura | |
| É a matriz ou uma cópia? | é a matriz |
| Estágio do Conteúdo | concluido |
| Transferível | 1 |
| Tipo do Conteúdo | External Contribution |
| Palavras-Chave | GEOLOGIA evolução tectono estratigráfia Provínvia Mineral de Carajás radar imageador tectonics stratigraphy evolution Carajás Mineral Province |
| Resumo | Orbital remote sensing images have been used in Carajás Mineral Province (Brazilian Amazon Region) since the beginning of the 1990s. The Province, with a heterogeneous relief and almost totally covered by tropical rainforest, is part of the Itacaiúnas Shear Belt within the Amazonian Craton. The area is world-wide known due to its mineral potential. However, from the tectono-stratigraphic viewpoint it is still problematic due to several drawbacks such as poor access, physiographic complexity, and detailed information available only in few isolated sites (mining, deposits or mineralizations). Spaceborne optical (Landsat TM) and radar (C-HH RADARSAT-1) imageries and digital integrated products (RADARSAT-1/Aerialgammaspectrometry) have been extensively applied for geological mapping purposes in the Province. Due to their synoptic view coupled with distinct sensor/terrain geometry allowing the extraction of indirect geological information, these kinds of remotely sensed products have been interpreted based on specific morphostructural criteria., with the following objectives: (1) to integrate previous and disperse geological data; (2) to explore the identification of regional structures and distinct tectonic-stratigraphic regimes on a large mapping scale; (3) to distinguish different motion phases along the Itacaiúnas Shear Belt (WNW-ESE trending) and characterize related rock forming and deformation events. Fieldwork campaigns carried out along selected profiles have provided new information. These findings were integrated with previous data and have allowed the production of a new tectono-stratigraphic map for the Province (1:250,000 scale). In addition, it was also possible to characterize three ductile and brittle transpression phases, locally transtensive, with Archean/Neoproterozoic ages. It was also observed extensive reactivations with pulses at the end of the Proterozoic and beginning of the Palaeozoic, at the Mesozoic and at the Tertiary. Volcanism, sedimentation, granitogenesis, metamorphism and deformation with distinct intensity are associated with these phases. The records of these deformations are clear in orbital remote sensing images and can be used as diagnostic of the distinct motion/deformation events in the Province. These orbital images are fundamental tools for tectono-stratigraphic mapping purposes in the Province. |
| Área | SRE |
| Arranjo | urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSR > A Evolução tectono-estratigráfica... |
| 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 | pt |
| Arquivo Alvo | evolução tectono.pdf |
| Grupo de Usuários | administrator banon marciana |
| Grupo de Leitores | administrator marciana |
| Visibilidade | shown |
| Detentor da Cópia | SID/SCD |
| Política de Arquivamento | denypublisher allowfinaldraft |
| Permissão de Leitura | deny from all and allow from 150.163 |
| Permissão de Atualização | não transferida |
| 5. Fontes relacionadas | |
| Unidades Imediatamente Superiores | 8JMKD3MGPCW/3ER446E |
| Divulgação | PORTALCAPES |
| Acervo Hospedeiro | sid.inpe.br/banon/2001/04.06.10.52 |
| 6. Notas | |
| Campos Vazios | affiliation alternatejournal archivist callnumber copyright creatorhistory descriptionlevel doi e-mailaddress electronicmailaddress format isbn label lineage mark mirrorrepository nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress rightsholder schedulinginformation secondarydate secondarymark session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url versiontype |
| 7. Controle da descrição | |
| e-Mail (login) | marciana |
| atualizar | |