| 1. Identificação | ||||
| Tipo de Referência | Artigo em Revista Científica (Journal Article) | |||
| Site | mtc-m21b.sid.inpe.br | |||
| Código do Detentor | isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S | |||
| Identificador | 8JMKD3MGP3W34P/3J33GL5 | |||
| Repositório | sid.inpe.br/mtc-m21b/2015/02.24.17.47 (acesso restrito) | |||
| Última Atualização | 2017:07.21.15.25.14 (UTC) simone | |||
| Repositório de Metadados | sid.inpe.br/mtc-m21b/2015/02.24.17.47.27 | |||
| Última Atualização dos Metadados | 2018:06.04.02.55.16 (UTC) administrator | |||
| DOI | 10.1130/2015.1212(16) | |||
| ISSN | 0072-1069 | |||
| Chave de Citação | CohenMcElZaSwAsSi:2015:SyMoAn | |||
| Título | Lake formation, characteristics, and evolution in retroarc deposystems: A synthesis of the modern Andean orogen and its associated basins  | |||
| Ano | 2015 | |||
| Data de Acesso | 02 maio 2024 | |||
| Tipo de Trabalho | journal article | |||
| Tipo Secundário | PRE PI | |||
| Número de Arquivos | 1 | |||
| Tamanho | 2820 KiB | |||
| 2. Contextualização | ||||
| Autor | 1 Cohen, Andrew 2 McGlue, Michael M. 3 Ellis, Geoffrey S. 4 Zani, Hiran 5 Swarzenski, Peter W. 6 Assine, Mario L. 7 Silva, Aguinaldo | |||
| Grupo | 1 2 3 4 DSR-OBT-INPE-MCTI-GOV-BR | |||
| Afiliação | 1 University of Arizona 2 Energy Resources Program 3 Energy Resources Program 4 Instituto Nacional de Pesquisas Espaciais (INPE) 5 U.S. Geological Survey 6 Universidade Estadual Paulista (UNESP) 7 Universidade Federal de Mato Grosso do Sul (UFMS) | |||
| Endereço de e-Mail do Autor | 1 cohen@email.arizona.edu 2 3 4 hzani@dsr.inpe.br | |||
| Revista | Memoir of the Geological Society of America | |||
| Volume | 212 | |||
| Páginas | 309-335 | |||
| Histórico (UTC) | 2015-02-24 17:47:27 :: simone -> administrator :: 2016-06-21 18:57:27 :: administrator -> simone :: 2015 2017-07-21 15:25:14 :: simone -> administrator :: 2015 2018-06-04 02:55:16 :: administrator -> simone :: 2015 | |||
| 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 | Climatic conditions Environmental signals Forward propagation Geochemical characteristic Rapid sedimentation Sediment generations Sedimentation rates Siliciclastic sediments | |||
| Resumo | Lake deposystems are commonly associated with retroarc mountain belts in the geological record. These deposystems are poorly characterized in modern retroarcs, placing limits on our ability to interpret environmental signals from ancient deposits. To address this problem, we have synthesized our existing knowledge about the distribution, morphometrics, and sedimentary geochemical characteristics of tectonically formed lakes in the central Andean retroarc. Large, active mountain belts such as the Andes frequently create an excess of sediment, to the point that modeling and observational data both suggest their adjacent retroarc basins will be rapidly overfilled by sediments. Lake formation, requiring topographic closure, demands special conditions such as topographic isolation and arid climatic conditions to reduce sediment generation, and bedrock lithologies that yield little siliciclastic sediment. Lacustrine deposition in the modern Andean retroarc has different characteristics in the six major morphotectonic zones discussed. (1) High-elevation hinterland basins of the arid Puna-Altiplano Plateau frequently contain underfilled and balanced-filled lakes that are potentially long-lived and display relatively rapid sedimentation rates. (2) Lakes are rare in piggyback basins, although a transition zone exists where basins that originally formed as piggybacks are transferred to the hinterland through forward propagation of the thrust belt. Here, lakes are moderately abundant and long-lived and display somewhat lower sedimentation rates than in the hinterland. (3) Wedge-top and (4) foredeep deposystems of the Andean retroarc are generally overfilled, and lakes are small and ephemeral. (5) Semihumid Andean backbulge basins contain abundant small lakes, which are moderately long-lived because of underfilling by sediment and low sedimentation rates. (6) Broken foreland lakes are common, typically underfilled, large, and long-lived playa or shallow systems. | |||
| Área | SRE | |||
| Arranjo | urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSR > Lake formation, characteristics,... | |||
| Conteúdo da Pasta doc | acessar | |||
| Conteúdo da Pasta source | não têm arquivos | |||
| Conteúdo da Pasta agreement |
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| 4. Condições de acesso e uso | ||||
| Idioma | en | |||
| Grupo de Usuários | simone | |||
| Grupo de Leitores | administrator simone | |||
| Visibilidade | shown | |||
| Permissão de Leitura | deny from all and allow from 150.163 | |||
| Permissão de Atualização | não transferida | |||
| 5. Fontes relacionadas | ||||
| Repositório Espelho | urlib.net/www/2011/03.29.20.55 | |||
| Unidades Imediatamente Superiores | 8JMKD3MGPCW/3ER446E | |||
| Lista de Itens Citando | ||||
| Divulgação | COMPENDEX; SCOPUS. | |||
| Acervo Hospedeiro | sid.inpe.br/mtc-m21b/2013/09.26.14.25.20 | |||
| 6. Notas | ||||
| Campos Vazios | alternatejournal archivingpolicy archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn label lineage mark month nextedition notes number orcid parameterlist parentrepositories previousedition previouslowerunit progress project resumeid rightsholder schedulinginformation secondarydate secondarykey secondarymark session shorttitle sponsor subject targetfile tertiarymark tertiarytype url | |||
| 7. Controle da descrição | ||||
| e-Mail (login) | simone | |||
| atualizar | ||||