@InProceedings{CremonRossZani:2012:GêEvGe,
               author = "Cremon, {\'E}dipo Henrique and Rossetti, Dilce de F{\'a}tima and 
                         Zani, Hiran",
          affiliation = "{} and {Instituto Nacional de Pesquisas Espaciais (INPE)}",
                title = "G{\^e}nese e evolu{\c{c}}{\~a}o geomorfol{\'o}gica do 
                         megaleque Demini (norte da Amaz{\^o}nia) baseado na an{\'a}lise 
                         morfoestrutural e hidroper{\'{\i}}odo",
            booktitle = "Anais...",
                 year = "2012",
         organization = "Simp{\'o}sio Nacional de Geomorfologia (SINAGEO), 9.",
             keywords = "megaleque Demini, Amaz{\^o}nia, hidroper{\'{\i}}odo, Demini 
                         megafan, Amazonia, hydroperiod.",
             abstract = "O objetivo desse trabalho foi de realizar a analise 
                         morfoestrutural do megaleque Demini, norte da Amaz{\^o}nia, e 
                         verificar suas poss{\'{\i}}veis rela{\c{c}}{\~o}es com 
                         {\'a}reas alagadas, visando estabelecer um modelo evolutivo 
                         geomorfol{\'o}gico. Para isso, baseou-se na an{\'a}lise 
                         morfol{\'o}gica de hidroper{\'{\i}}odo e 
                         interpreta{\c{c}}{\~a}o de anomalias e lineamentos 
                         morfoestruturais. Conclui-se que subsid{\^e}ncia regional criou 
                         depress{\~a}o com subsequente preenchimento sedimentar e 
                         forma{\c{c}}{\~a}o do sistema deposicional com extensa {\'a}rea 
                         alag{\'a}vel. ABSTRACT: The aim of this work was to perform the 
                         Demini megafan morphostructural analysis, northern Amazonia, and 
                         verify their possible relationships with wetlands, to establish a 
                         model geomorphological evolution. For this, it was based on 
                         morphological analysis and interpretation of hydroperiod and 
                         morphostructural lineaments. The data indicated that regional 
                         subsidence created depression with subsequent formation of 
                         sedimentary fill by megafan with extensive flooded area.",
  conference-location = "Rio de Janeiro",
      conference-year = "21-24 de Outubro de 2012",
                label = "lattes: 7888258901938956 1 CremonRossZani:2012:G{\^e}EvGe",
             language = "pt",
           targetfile = "2-440-165.pdf",
        urlaccessdate = "30 abr. 2024"
}