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@PhDThesis{AlmeidaFo:1983:CoMe,
               author = "Almeida Filho, Raimundo",
                title = "Sensoriamento remoto orbital aplicado {\`a} 
                         prospec{\c{c}}{\~a}o mineral nas prov{\'{\i}}ncias 
                         estan{\'{\i}}feras de Goi{\'a}s e Rond{\^o}nia: uma 
                         contribui{\c{c}}{\~a}o metodol{\'o}gica",
               school = "Universidade de S{\~a}o Paulo",
                 year = "1983",
              address = "S{\~a}o Paulo",
                month = "1983",
             keywords = "geologia, Goi{\'a}s (estado), Rond{\^o}nia (estado), 
                         prospec{\c{c}}{\~a}o mineral, geology, estanho, mineral 
                         prospection, tin.",
             abstract = "Discute-se neste trabalho uma linha metodol{\'o}gica de 
                         utiliza{\c{c}}{\~a}o de dados de sensoriamento remoto orbital, 
                         como ferramenta de auxilio a campanhas de prospec{\c{c}}{\~a}o 
                         mineral, exemplificada no estudo de corpos gran{\'{\i}}ticos das 
                         Prov{\'{\i}}ncias Estan{\'{\i}}feras de Goi{\'a}s e de 
                         Rond{\^o}nia. Inicialmente faz-se uma discuss{\~a}o do papel de 
                         diversos par{\^a}metros que interagem para compor o sinal gravado 
                         pelos sistemas sensores. S{\~a}o par{\^a}metros fundamentais no 
                         processo de an{\'a}lise e interpreta{\c{c}}{\~a}o de dados 
                         multispectrais em geologia: as caracter{\'{\i}}sticas 
                         fisiogr{\'a}ficas da regi{\~a}o; as caracter{\'{\i}}sticas 
                         geol{\'o}gicas do {"}alvo{"} pesquisado; o papel das 
                         vari{\'a}veis sazonais (cobertura vegetal e condi{\c{c}}{\~o}es 
                         de ilumina{\c{c}}{\~a}o); as caracter{\'{\i}}sticas do sistema 
                         sensor (resolu{\c{c}}{\~o}es); e as t{\'e}cnicas de realce de 
                         imagens digitais atrav{\'e}s do emprego de computadores. A 
                         utiliza{\c{c}}{\~a}o de imagens digitais/multispectrais do 
                         sensor MSS-LANDSAT, levando em considera{\c{c}}{\~a}o todos os 
                         aspectos acima, permitiu a discrimina{\c{c}}{\~a}o de {\'a}reas 
                         de ocorr{\^e}ncias de f{\'a}ceis greisenizadas ({"}lato 
                         sensu{"}) associadas a corpos gran{\'{\i}}ticos da 
                         Prov{\'{\i}}ncia Estan{\'{\i}}fera de Goi{\'a}s, as quais 
                         s{\~a}o controles litol{\'o}gicos de mineraliza{\c{c}}{\~o}es 
                         de Sn, W, Nb-Ta, Li, F, etc. O par{\^a}metro b{\'a}sico que 
                         permitiu a discrimina{\c{c}}{\~a}o destas areas atrav{\'e}s de 
                         imagens orbitais foi o comportamento espectral destes tipos 
                         litol{\'o}gicos e/ou de suas associa{\c{c}}{\~o}es 
                         espec{\'{\i}}ficas de rocha-solo-vegeta{\c{c}}{\~a}o. Em 
                         Rond{\^o}nia, dadas as caracter{\'{\i}}sticas da regi{\~a}o 
                         (profundo manto de intemperismo, coberturas sedimentares 
                         quatern{\'a}rias e floresta tropical), n{\~a}o {\'e} 
                         poss{\'{\i}}vel a discrimina{\c{c}}{\~a}o espectral de 
                         litotipos espec{\'{\i}}ficos. No entanto, mesmo sob essas 
                         condi{\c{c}}{\~o}es, a imagem LANDSAT real{\c{c}}ada por 
                         computador, mostrou os tra{\c{c}}os geol{\'o}gicos principais e 
                         a estrutura{\c{c}}{\~a}o do maci{\c{c}}o gran{\'{\i}}tico 
                         estudado, fei{\c{c}}{\~o}es estas n{\~a}o observadas 
                         atrav{\'e}s de fotografias a{\'e}reas ou de imagens de RADAR. Os 
                         resultados obtidos em Goi{\'a}s e em Rond{\^o}nia mostram que a 
                         utiliza{\c{c}}{\~a}o adequada de imagens de sensoriamento remoto 
                         orbital pode contribuir de maneira efetiva na 
                         orienta{\c{c}}{\~a}o a trabalhos de prospec{\c{c}}{\~a}o 
                         mineral, propiciando economias razo{\'a}veis de tempo e de 
                         recursos na etapa de levantamentos de campo. ABSTRACT: This study 
                         presents a line of procedures for the utilization of orbital 
                         remote sensing data as supporting tools in mineral prospecting 
                         campaigns, exemplified here by studies in granitic bodies of the 
                         Tin Provinces of Goi{\'a}s and Rond{\^o}nia. Initially, a 
                         discussion is made on the role of several interacting parameters 
                         that compose the recorded signal in sensor systems. The 
                         fundamental parameters in the processes of analysis and 
                         interpretation of multispectral data in geology are: the 
                         physiographic characteristics of the region; the geological 
                         characteristics of the target investigated; the role of the 
                         seasonal variables (vegetation cover and illumination conditions); 
                         the characteristics of the sensor system (resolutions); and the 
                         use of computer enhancement techniques applied to digital images. 
                         Taking into consideration the above aspects, the utilization of 
                         LANDSAT multispectral/digital images has allowed the 
                         discrimination of areas with occurrences of greisenized facies 
                         ({"}lato sensu{"}) associated to the granitic massifs in the 
                         Goi{\'a}s Tin Province. The greisens are lithological controls of 
                         mineralizations in Sn, W, Nb-Ta, Li, F, and others. The basic 
                         parameter that allowed the discrimination of these areas in 
                         orbital images was the spectral behaviour of these lithological 
                         types and/or of their specific rock-soil-vegetation associations. 
                         In Rond{\^o}nia, due to the particular characteristics of the 
                         region (deep weathering, Quaternary sedimentary covers, and 
                         Tropical Forest), a spectral discrimination of specific lithotypes 
                         is not possible. However, even under these adverse conditions, 
                         computer enhanced LANDSAT images showed the main geological and 
                         structural features of the studied granitic massif. These were not 
                         observed in aerial photography or RADAR images. The results 
                         obtained in Goi{\'a}s and Rond{\^o}nia show that an adequate 
                         utilization of orbital remote sensing images can contribute for 
                         the orientation of field work, yielding reasonable saving in time 
                         and resources during mineral prospecting campaigns.",
          affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)}",
            committee = "Amaral, Gilberto and Damasceno, Eduardo Camilher and Bettencourt, 
                         Jorge Silva and Vitorello, Icaro and Ribeiro Filho, Evaristo",
           copyholder = "SID/SCD",
         englishtitle = "Mineral prospecting bodies in granitic of estaniferas provincial 
                         in Goi{\'a}s and Rond{\^o}nia: a methodological contribution",
                label = "1075",
             language = "pt",
                pages = "171",
           targetfile = "publicacao.pdf",
        urlaccessdate = "07 maio 2024"
}


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