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@InProceedings{AndradesFoRossBeze:2015:GeAeIn,
               author = "Andrades Filho, Cl{\'o}dis de Oliveira and Rossetti, Dilce de 
                         F{\'a}tima and Bezerra, Francisco Hil{\'a}rio Rego",
          affiliation = "{} and {Instituto Nacional de Pesquisas Espaciais (INPE)}",
                title = "Geomorfometria e aeromagnetometria integradas para an{\'a}lise da 
                         correspond{\^e}ncia entre lineamentos morfoestruturais e 
                         magn{\'e}ticos na Bacia Para{\'{\i}}ba, nordeste do Brasil",
            booktitle = "Anais...",
                 year = "2015",
               editor = "Gherardi, Douglas Francisco Marcolino and Arag{\~a}o, Luiz 
                         Eduardo Oliveira e Cruz de",
                pages = "3384--3391",
         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 = "The northeast region of Brazil has been the target of studies 
                         which have shown the relevance of seismic events in recent 
                         geological times; however, the genesis of these events is still 
                         unknown. This work integrates geomorphometric data derived from 
                         interferometric radar and aerogeophysical magnetic data for the 
                         analysis of spatial and directional relationship between 
                         morphostructural and magnetic lineaments in the Para{\'{\i}}ba 
                         Basin, northeastern Brazil. The objective is to evaluate the 
                         correspondence between the deep tectonic structures in the 
                         subsurface, and the features, observed through the relief, on the 
                         surface. Geomorphometric products were used for extracting 
                         morphostructural lineaments, such as aspect, horizontal curvature 
                         and altimetry. Data regarding the anomalous magnetic field and the 
                         so-called product first vertical derivative were used for 
                         detection of magnetic lineaments. From the analysis performed 
                         using the Geographic Information System SPRING 5.2, it was 
                         possible to identify important spatial and directional 
                         correspondences which enables proposing that areas of pre-existing 
                         shear in the study area were reactivated in the Cenozoic, more 
                         specifically in the Late Quaternary. This is proposed due to the 
                         similarity between the main orientations of lineaments E-W, NE-SW 
                         and NW-SE of sedimentary units and the area of the Precambrian 
                         basement. In addition, the geographical distribution of magnetic 
                         and morphostructural lineaments shows strong correspondence, 
                         particularly along major rivers and valleys of central onshore 
                         portion of the Para{\'{\i}}ba Basin.",
  conference-location = "Jo{\~a}o Pessoa",
      conference-year = "25-29 abr. 2015",
                 isbn = "978-85-17-0076-8",
                label = "672",
             language = "pt",
         organisation = "Instituto Nacional de Pesquisas Espaciais (INPE)",
                  ibi = "8JMKD3MGP6W34M/3JM4BKT",
                  url = "http://urlib.net/rep/8JMKD3MGP6W34M/3JM4BKT",
           targetfile = "p0672.pdf",
                 type = "Geologia",
        urlaccessdate = "30 nov. 2020"
}


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