@InProceedings{AndradesFoRoss:2012:GeInTe,
               author = "Andrades Filho, Clodis de Oliveira and Rossetti, Dilce de 
                         F{\'a}tima",
          affiliation = "{Universidade de S{\~a}o Paulo (USP)} and {Instituto Nacional de 
                         Pesquisas Espaciais (INPE)}",
                title = "Geomorfometria e intensidade tect{\^o}nica na por{\c{c}}{\~a}o 
                         emersa da bacia Para{\'{\i}}ba – nordeste do Brasil",
            booktitle = "Anais...",
                 year = "2012",
         organization = "Simp{\'o}sio Nacional de Geomorfologia (SINAGEO), 9.",
             keywords = "quatern{\'a}rio, deforma{\c{c}}{\~o}es tect{\^o}nicas, 
                         Forma{\c{c}}{\~a}o Barreiras, quaternary, tectonic deformation, 
                         Barreiras Formation.",
             abstract = "Este estudo aplica {\'{\i}}ndices morfom{\'e}tricos na 
                         avalia{\c{c}}{\~a}o da intensidade tect{\^o}nica na 
                         por{\c{c}}{\~a}o emersa da Bacia Sedimentar Para{\'{\i}}ba a 
                         partir dos dados: rede de drenagem e modelo digital de 
                         eleva{\c{c}}{\~a}o. Os {\'{\i}}ndices rela{\c{c}}{\~a}o 
                         declividade-extens{\~a}o (RDE), fator assim{\'e}trico (Af), 
                         integral hipsom{\'e}trica (Hi) e sinuosidade de frente de 
                         montanha (Smf) possibilitaram distinguir diferentes intensidades 
                         de deforma{\c{c}}{\~a}o. Destaca-se a por{\c{c}}{\~a}o NE da 
                         {\'a}rea, onde {\'e} sugerido tectonismo mais intenso no 
                         Ne{\'o}geno e Quatern{\'a}rio. ABSTRACT: This study applies 
                         morphometric indices in the evaluation of tectonic intensity in 
                         the onshore portion of the Para{\'{\i}}ba Sedimentary Basin 
                         using the following data: drainage network and digital elevation 
                         model. The indices slope-length ratio (SL), asymmetric factor 
                         (Af), hypsometric integral (Hi) and mountain-front sinuosity (Smf) 
                         enabled us to distinguish different intensities of deformation. We 
                         highlight the NE portion of the area, where more intense tectonism 
                         is suggested in Neogene-Quaternary.",
  conference-location = "Rio de Janeiro",
      conference-year = "21-24, Outubro, 2012",
                label = "lattes: 0307721738107549 2 AndradesFoRoss:2012:GEINTE",
             language = "pt",
           targetfile = "8-321-477.pdf",
        urlaccessdate = "30 abr. 2024"
}