@InProceedings{PavãoRoiMenFraAlv:2011:MeInEs,
               author = "Pav{\~a}o, Cesar Garcia and Roig, Henrique Llacer and Menezes, 
                         Paulo Henrique Bretanha Junker and Fran{\c{c}}a, George Sand 
                         Le{\~a}o Ara{\'u}jo de and Alves, Ruan Roussenq",
          affiliation = "{Universidade de Bras{\'{\i}}lia - UnB} and {Universidade de 
                         Bras{\'{\i}}lia - UnB} and {Universidade de Bras{\'{\i}}lia - 
                         UnB} and {Universidade de Bras{\'{\i}}lia - UnB} and 
                         {Universidade de Bras{\'{\i}}lia - UnB}",
                title = "Metodologias de interpola{\c{c}}{\~a}o espacial aplicada a dados 
                         de espessura crustal na Bacia do Paran{\'a}",
            booktitle = "Anais...",
                 year = "2011",
               editor = "Epiphanio, Jos{\'e} Carlos Neves and Galv{\~a}o, L{\^e}nio 
                         Soares",
                pages = "3435--3442",
         organization = "Simp{\'o}sio Brasileiro de Sensoriamento Remoto, 15. (SBSR).",
            publisher = "Instituto Nacional de Pesquisas Espaciais (INPE)",
              address = "S{\~a}o Jos{\'e} dos Campos",
             keywords = "espessura crustal, interpola{\c{c}}{\~a}o espacial, Bacia do 
                         Paran{\'a}.",
             abstract = "The use of methods of spatial interpolation of data is becoming 
                         increasingly common in geophysical analysis, because of that, 
                         currently, several software already contain a lot of these 
                         methods, allowing more detailed studies. In the present work to 
                         evaluate three methods of interpolation data for crustal thickness 
                         of the Paran{\'a} Basin, with the intention of making a map of 
                         the Moho for the region. The methods are IDW, Spline and Kriging. 
                         We compiled 39 data that were a database and analyzed using the 
                         software ArcGIS 9.3. The results showed a thicker crust in the 
                         central part with thinning to the edge. Traditional methods, IDW 
                         and Spline in its results generate anomalies not compatible with 
                         the 2.0 model crust. The analysis results of geostatistical 
                         Kriging are more refined and consistent, showing no abnormalities 
                         point, besides showing more consistent compared with the model, 
                         except the northwest, where there is a mismatch between the models 
                         due to data exclusivity of gravity, which are less precise than 
                         the data of receiver function and seismic.",
  conference-location = "Curitiba",
      conference-year = "30 abr. - 5 maio 2011",
                 isbn = "{978-85-17-00056-0 (Internet)} and {978-85-17-00057-7 (DVD)}",
             language = "pt",
         organisation = "Instituto Nacional de Pesquisas Espaciais (INPE)",
                  ibi = "3ERPFQRTRW/3A356HS",
                  url = "http://urlib.net/ibi/3ERPFQRTRW/3A356HS",
           targetfile = "p1233.pdf",
                 type = "Geologia",
        urlaccessdate = "12 maio 2024"
}