@InProceedings{CarvalhoSilv:2005:ApTéPr,
               author = "Carvalho, J{\'u}lio Alexandre Almeida de and Silva, Fernando 
                         Cesar Alves da",
          affiliation = "{Universidade Federal do Rio Grande do Norte (UFRN)} and 
                         {Universidade Federal do Rio Grande do Norte (UFRN)}",
                title = "Aplica{\c{c}}{\~a}o de t{\'e}cnicas de processamento digital de 
                         imagens para a caracteriza{\c{c}}{\~a}o do padr{\~a}o dos 
                         lineamentos fr{\'a}geis na regi{\~a}o de Santana do Acara{\'u} 
                         - CE",
            booktitle = "Anais...",
                 year = "2005",
               editor = "Epiphanio, Jos{\'e} Carlos Neves and Fonseca, Leila Maria 
                         Garcia",
                pages = "1717--1724",
         organization = "Simp{\'o}sio Brasileiro de Sensoriamento Remoto, 12. (SBSR)",
            publisher = "INPE",
              address = "S{\~a}o Jos{\'e} dos Campos",
             keywords = "brittle deformation, remote sensing, lineaments, 
                         deforma{\c{c}}{\~a}o fr{\'a}gil, sensoriamento remoto, 
                         lineamentos.",
             abstract = "This work focused the brittle deformation of a siliciclastic body 
                         (sandstone with conglomeration) outcropping near Santana do 
                         Acara{\'u} city (Cear{\'a}-state, Brasil), and it basement 
                         (mainly gneissic rocks). By using Landsat images the lineaments 
                         were identified and classified according to their directions. A 
                         terrain digital model was built and stressed the information of 
                         the faults controlling the geometry of the siliciclastic body. The 
                         brittle deformation is interpreted as due to a high crustal level 
                         reactivation of a mega ductile sheer zone known as Sobral-Pedro-II 
                         lineament. This area is taken as analogous of the deformation 
                         acting also in the basins of the Brazilian equatorial margin.",
  conference-location = "Goi{\^a}nia",
      conference-year = "16-21 abr. 2005",
                 isbn = "85-17-00018-8",
             language = "Portugu{\^e}s",
         organisation = "Instituto Nacional de Pesquisas Espaciais",
                  ibi = "ltid.inpe.br/sbsr/2004/11.21.14.45",
                  url = "http://urlib.net/ibi/ltid.inpe.br/sbsr/2004/11.21.14.45",
           targetfile = "1717.pdf",
                 type = "Geologia",
        urlaccessdate = "12 maio 2024"
}