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@MastersThesis{AndradesFo:2010:AnMoPo,
               author = "Andrades Filho, Cl{\'o}dis de Oliveira",
                title = "An{\'a}lise morfoestrutural da por{\c{c}}{\~a}o central da 
                         Bacia Para{\'{\i}}ba (PB) a partir de dados MDE-SRTM e 
                         ALOS-PALSAR FBD",
               school = "Instituto Nacional de Pesquisas Espaciais (INPE)",
                 year = "2010",
              address = "S{\~a}o Jos{\'e} dos Campos",
                month = "2010-04-28",
             keywords = "MDE-SRTM, ALOS-PALSAR, lineamentos morfoestruturais, 
                         {\'{\i}}ndices morfom{\'e}tricos, Bacia Para{\'{\i}}ba (PB), 
                         DEM-SRTM, ALOS-PALSAR, morphostructural lineaments, morphometric 
                         indices, Paraiba Basin (PB).",
             abstract = "A presente pesquisa objetivou a an{\'a}lise morfoestrutural da 
                         por{\c{c}}{\~a}o central da Bacia Para{\'{\i}}ba (PB), por 
                         meio da integra{\c{c}}{\~a}o de informa{\c{c}}{\~o}es 
                         qualitativas (i.e., densidade e direcionamento de lineamentos 
                         morfoestruturais; padr{\~o}es e anomalias de drenagem) e 
                         quantitativas (i.e., {\'{\i}}ndices morfom{\'e}tricos), a fim 
                         de verificar se a evolu{\c{c}}{\~a}o da drenagem e do relevo 
                         ocorreu sob influ{\^e}ncia tect{\^o}nica. A 
                         investiga{\c{c}}{\~a}o incluiu dados de sensoriamento remoto 
                         derivados do MDE (modelo digital de eleva{\c{c}}{\~a}o)-SRTM 
                         (Shuttle Radar Topography Mission) e do sistema radar ALOS 
                         (Advanced Land Observing Satellite)-PALSAR (Phased Array type 
                         L-band Synthetic Aperture), al{\'e}m de base de drenagem digital 
                         extra{\'{\i}}dos de cartas topogr{\'a}ficas da DSG (Diretoria 
                         de Servi{\c{c}}o Geogr{\'a}fico). Al{\'e}m de auxiliar na 
                         extra{\c{c}}{\~a}o de lineamentos morfoestruturais, o MDE-SRTM 
                         serviu, tamb{\'e}m, de suporte {\`a} an{\'a}lise da rede de 
                         drenagem e {\`a} aplica{\c{c}}{\~a}o de {\'{\i}}ndices 
                         morfom{\'e}tricos. Os resultados revelaram que o MDE-SRTM foi 
                         mais eficiente para salientar lineamentos morfoestruturais do que 
                         o PALSAR. Caracter{\'{\i}}sticas geom{\'e}tricas de 
                         obten{\c{c}}{\~a}o das imagens PALSAR e a interfer{\^e}ncia da 
                         cobertura do solo contribu{\'{\i}}ram para ocultar ou suavizar 
                         as morfoestruturas neste produto. Os lineamentos morfoestruturais 
                         extra{\'{\i}}dos do MDE-SRTM tiveram boa correspond{\^e}ncia 
                         com estruturas tect{\^o}nicas registradas na {\'a}rea de estudo. 
                         Outros ind{\'{\i}}cios de influ{\^e}ncia tect{\^o}nica 
                         incluem: elevada freq{\"u}{\^e}ncia de padr{\~o}es de drenagem 
                         treli{\c{c}}a (e suas varia{\c{c}}{\~o}es); ocorr{\^e}ncia de 
                         padr{\~a}o retangular angular; e abund{\^a}ncia de anomalias de 
                         drenagem, principalmente, em {\'a}reas dominadas por cobertura 
                         sedimentar. Adicionalmente, os {\'{\i}}ndices morfom{\'e}tricos 
                         mostraram, em geral, valores condizentes com influ{\^e}ncia 
                         tect{\^o}nica. Os {\'{\i}}ndices tamb{\'e}m indicaram que a 
                         por{\c{c}}{\~a}o nordeste da {\'a}rea com dom{\'{\i}}nio de 
                         cobertura sedimentar e o setor norte da {\'a}rea com 
                         dom{\'{\i}}nio do embasamento cristalino foram os que 
                         registraram maior intensidade de atividade tect{\^o}nica em 
                         tempos geol{\'o}gicos mais recentes. Os dados qualitativos e 
                         quantitativos derivados do MDE-SRTM forneceram evid{\^e}ncias em 
                         suporte {\`a} influ{\^e}ncia tect{\^o}nica na {\'a}rea de 
                         estudo. Deforma{\c{c}}{\~a}o r{\'u}ptil e d{\'u}ctil 
                         decorrente da reativa{\c{c}}{\~a}o de falhas tect{\^o}nicas 
                         precambrianas durante o Mesoz{\'o}ico e Cenoz{\'o}ico e 
                         gera{\c{c}}{\~a}o de novas estruturas durante estes 
                         per{\'{\i}}odos, foram fundamentais na defini{\c{c}}{\~a}o da 
                         paisagem e no controle dos padr{\~o}es de 
                         sedimenta{\c{c}}{\~a}o na parte central da Bacia 
                         Para{\'{\i}}ba. ABSTRACT: The present study aimed the 
                         morphostructural analysis of the central portion of the 
                         Para{\'{\i}}ba Basin (PB) through integration of qualitative 
                         (i.e., density and direction of morphostructural lineaments; 
                         drainage patterns and anomalies) and quantitative morphometric 
                         indices) information in order to test if drainage and relief 
                         evolved under the influence of tectonics. The investigation 
                         included remote sensing data derived from both DEM (digital 
                         elevation model)-SRTM (Shuttle Radar Topography Mission) and ALOS 
                         (Advanced Land Observing Satellite)-PALSAR (Phased Array type 
                         L-band Synthetic Aperture) radar system, as well as digital 
                         drainage data extracted from DSG (Department of Geographical 
                         Service) topographic maps. In addition to help extracting the 
                         morphostructural lineaments, the DEM-SRTM also provided the basis 
                         to analyse the drainage network and to apply the morphometric 
                         indexes. The results revealed that the DEM-SRTM was more efficient 
                         to enhance the morphostructural lineaments than the PALSAR. 
                         Geometric characteristics during acquisition of PALSAR data and 
                         land cover interference contributed to obliterate or mask the 
                         morphostructures in this product. The morphostructural lineaments 
                         derived from the DEM-SRTM had good correspondence with tectonic 
                         structures recorded in the study area. Other evidence of tectonic 
                         influence include: high frequency of trellis drainage patterns 
                         (and their variations); occurrence of angular-rectangular pattern; 
                         and abundance of drainage anomalies, mainly in areas dominated by 
                         sedimentary cover. Additionally, the morphometric indexes showed, 
                         in general, values consistent with tectonic influence. The indexes 
                         also indicated that the northeast area with dominance of 
                         sedimentary cover and the northern sector of the area with 
                         dominance of crystalline basement were the ones with the greatest 
                         intensity in tectonic activity in more recent geological times. 
                         The qualitative and quantitative information derived from the 
                         DEM-SRTM provided evidence in support of tectonic influence in the 
                         study area. Both brittle and ductile deformations related to 
                         reactivation of Precambrian tectonic faults during the Mesozoic 
                         and the Cenozoic, added to creation of new features during these 
                         periods, were crucial to define the landscape and to control 
                         sedimentation patterns in the central Para{\'{\i}}ba Basin.",
            committee = "Paradella, Waldir Renato (presidente) and Rossetti, Dilce de 
                         F{\'a}tima (orientador) and Valeriano, M{\'a}rcio de Morisson 
                         and Bezerra, Francisco Hil{\'a}rio Rego",
           copyholder = "SID/SCD",
         englishtitle = "Morphostructural analysis on the central portion of 
                         Para{\'{\i}}ba Basin (PB) using DEM-SRTM and ALOS-PALSAR FBD 
                         data",
             language = "pt",
                pages = "173",
                  ibi = "8JMKD3MGP7W/37A6Q4S",
                  url = "http://urlib.net/ibi/8JMKD3MGP7W/37A6Q4S",
        urlaccessdate = "28 abr. 2024"
}


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