@InProceedings{RossettiValBezBriGóe:2009:CoCoAr,
               author = "Rossetti, Dilce de F{\'a}tima and Valeriano, M{\'a}rcio de 
                         Morisson and Bezerra, Francisco Hil{\'a}rio Rego and Brito Neves, 
                         Benjamim Bley and G{\'o}es, Ana Maria",
          affiliation = "INPE and INPE and UFRN and USP and USP",
                title = "Caracteriza{\c{c}}{\~a}o morfol{\'o}gica da por{\c{c}}{\~a}o 
                         sul da Sub-bacia de Alhandra, Bacia Para{\'{\i}}ba, com base em 
                         dados SRTM: contribui{\c{c}}{\~a}o na compreens{\~a}o do 
                         arcabou{\c{c}}o estrutural",
            booktitle = "Anais...",
                 year = "2009",
               editor = "Epiphanio, Jos{\'e} Carlos Neves and Galv{\~a}o, L{\^e}nio 
                         Soares",
                pages = "3325--3332",
         organization = "Simp{\'o}sio Brasileiro de Sensoriamento Remoto, 14. (SBSR)",
            publisher = "Instituto Nacional de Pesquisas Espaciais (INPE)",
              address = "S{\~a}o Jos{\'e} dos Campos",
             keywords = "tect{\^o}nica, morfologia, dobra, cenoz{\'o}ico, drenagem, 
                         Sub-bacia Alhandra.",
             abstract = "Features related to tectonic faults in deposits of the Barreiras 
                         Formation have been increasingly recorded in the literature. 
                         However, the record of deformation structures associated to folds 
                         in this unit is rare. This work aims to demonstrate that the 
                         Barreiras Formation in the south of the Alhandra Sub-Basin shows 
                         peculiar terrain characteristics, expressed by morphological and 
                         drainage anomalies that conform to the presence of both faults and 
                         folds. These features, extracted from SRTM digital elevation data, 
                         mostly include the prevalence of trellis drainage pattern and of 
                         rivers that change rapidly their courses according to curved 
                         trajectories. Field work confirms the presence of anticlines in 
                         the Barreiras Formation, probably developed due to NS compression 
                         during the Pliocene-Pleistocene.",
  conference-location = "Natal",
      conference-year = "25-30 abr. 2009",
                 isbn = "978-85-17-00044-7",
             language = "pt",
         organisation = "Instituto Nacional de Pesquisas Espaciais (INPE)",
                  ibi = "dpi.inpe.br/sbsr@80/2008/11.14.09.38",
                  url = "http://urlib.net/ibi/dpi.inpe.br/sbsr@80/2008/11.14.09.38",
           targetfile = "3325-3332.pdf",
                 type = "Geologia",
        urlaccessdate = "12 maio 2024"
}