@InProceedings{LimaBeRoVaAnAr:2015:AnMoBa,
               author = "Lima, Jean Carlos Ferreira de and Bezerra, Francisco Hil{\'a}rio 
                         Rego and Rossetti, Dilce de F{\'a}tima and Vasconcelos, David 
                         Lino and Andrades Filho, Cl{\'o}dis de Oliveira and Ara{\'u}jo, 
                         Renata Emily Brito de",
          affiliation = "{} and {} and {Instituto Nacional de Pesquisas Espaciais (INPE)}",
                title = "An{\'a}lise morfoestrutural da Bacia Para{\'{\i}}ba com radar 
                         interferom{\'e}trico",
            booktitle = "Anais...",
                 year = "2015",
               editor = "Gherardi, Douglas Francisco Marcolino and Arag{\~a}o, Luiz 
                         Eduardo Oliveira e Cruz de",
                pages = "567--573",
         organization = "Simp{\'o}sio Brasileiro de Sensoriamento Remoto, 17. (SBSR)",
            publisher = "Instituto Nacional de Pesquisas Espaciais (INPE)",
              address = "S{\~a}o Jos{\'e} dos Campos",
             abstract = "Passive continental margins are theoretically considered stable. 
                         However, several studies have shown that the northeastern margin 
                         of the South American continental plate presents signs of Cenozoic 
                         and Quaternary tectonic reactivations. This issue may be 
                         investigated using morphostructural analysis. In this work we 
                         mapped morphostructural lineaments from a selected area located in 
                         the south central portion of the Para{\'{\i}}ba Basin, 
                         northeastern Brazil, with the main objective of understanding how 
                         neotectonic processes influenced the morphology and sedimentation 
                         in this basin. The linear elements were extracted by analysis of 
                         interferometric radar C-band data from the TOPODATA/INPE database, 
                         which is a derivation of the digital elevation model (DEM) 
                         provided by the Shuttle Radar Topography Mission (SRTM). 
                         Processing included application of a directional filter at 
                         different azimuths to highlight the morphotectonic lineaments in 
                         different directions with the use of the software ArcMap 9.3. The 
                         result indicated that the lineaments mapped over the sedimentary 
                         units trend in the same direction than several structural 
                         lineaments of the basement shear zones. The three main trends are 
                         related to reactivation of NE-SW, NW-SE and EW trending faults 
                         during the Quaternary and Miocene.",
  conference-location = "Jo{\~a}o Pessoa",
      conference-year = "25-29 abr. 2015",
                 isbn = "978-85-17-0076-8",
                label = "110",
             language = "pt",
         organisation = "Instituto Nacional de Pesquisas Espaciais (INPE)",
                  ibi = "8JMKD3MGP6W34M/3JM45EB",
                  url = "http://urlib.net/ibi/8JMKD3MGP6W34M/3JM45EB",
           targetfile = "p0110.pdf",
                 type = "Geologia",
        urlaccessdate = "27 abr. 2024"
}