@MastersThesis{Almeida:1983:PrSuCo,
               author = "Almeida, Teodoro Isnard Ribeiro de",
                title = "O arco de Ponta Grossa: uma proposta para a sua 
                         configura{\c{c}}{\~a}o e evolu{\c{c}}{\~a}o a partir da 
                         interpreta{\c{c}}{\~a}o de dados de sensoriamento remoto",
               school = "Instituto Nacional de Pesquisas Espaciais (INPE)",
                 year = "1983",
              address = "Sao Jose dos Campos",
                month = "1982-06-24",
             keywords = "geologia, Arco de Ponta Grossa, arqueamento, evolu{\c{c}}{\~a}o 
                         de arco, {\'a}pice de arco, tectonica de sin{\'e}clise, 
                         magnetismo b{\'a}sico e alcalino, geology, Arch of Ponta Grossa, 
                         arching, arc evolution, arc apex, syneclysis tectonica, basic and 
                         alkaline magnetism.",
             abstract = "A an{\'a}lise visual de cinco cenas MSS-LANDSAT forneceu um mapa 
                         de diques fotointerpretados com o aux{\'{\i}}lio de m{\'e}todos 
                         fotogr{\'a}ficos e de computa{\c{c}}{\~a}o. Desse modo, foi 
                         poss{\'{\i}}vel definir a zona de maior densidade de diques e os 
                         aspectos de sua heterogeneidade, bem como propor a 
                         localiza{\c{c}}{\~a}o do {\'a}pice do arqueamento. Aventou-se 
                         como limite sul o Alinhamento de Iva{\'{\i}}, ora definido 
                         preliminarmente a partir das Imagens MSS-LANDSAT, tendo-se suposto 
                         como limite norte o Alinhamento de Guapiara, j{\'a} definido na 
                         literatura. Baseando-se em mapas de is{\'o}pacas de v{\'a}rias 
                         unidades estratigr{\'a}ficas da Bacia do Paran{\'a}, nas 
                         propostas ora feitas, e na proposta do Alinhamento de Guapiara, 
                         procurou-se esbocar a evolu{\c{c}}{\~a}o do Arco de Ponta Grossa 
                         desde o Devoniano ate o Juro-Cret{\'a}ceo. Na an{\'a}lise deste 
                         conjunto de informa{\c{c}}{\~o}es p{\^o}de-se observar alguns 
                         aspectos interessantes, entre os quais o aparente sincronismo 
                         entre a atividade da Bacia do Paran{\'a} e do Arco de Ponta 
                         Grossa, e o car{\'a}ter oposto entre os movimentos verticais da 
                         zona do {\'a}pice e dos Alinhamentos de Guapiara e Iva{\'{\i}}. 
                         ABSTRACT: A map of dikes was drawn up based on the visual analysis 
                         of MSS-LANDSAT images. It includes a wide area under the influence 
                         of the Ponta Grossa Arch both in the Paran{\'a} Basin and its 
                         basement. The analysis of this map by means of phtographic methods 
                         - greatly reduced for condensation of information and computation 
                         - statistical treatmen for the directions of the intrusive rocks - 
                         made it possible to define the zone of highest density of the 
                         dikes and some aspects of the longitudinal and transverse 
                         heterogeneities, as well as to localize the apex of the Arch. With 
                         regard to the boarder lines of the Ponta Grossa Arch we have put 
                         foward the suggestion of the Iva{\'{\i}} structural Alignment as 
                         the southern boarder, while the northern boarder has been taken to 
                         be the Guapiara structural Alignment as proposed in another paper. 
                         Field works were carried out for the purpose of confirming the 
                         suggested position of the apex of the flexure on Paleozoic 
                         sediments and pre-lava Mesozoic sediments. Furthermore, 
                         controversial aspects of the relative absence of dikes in certain 
                         units or lithologies and the composition of the intrusions 
                         surrounding the city of Castro (PR) were also observed. According 
                         to isopach maps fo different units of the Paran{\'a} Basin and 
                         the above mentioned proposals, an outline of the evolution of the 
                         Arch from the Devonian to the Juro-Cretaceous period was built up. 
                         It was thus possible to deduce several observations such as the 
                         apparent synchronism between the activity of the Paran{\'a} Basin 
                         and the Ponta Grossa Arch, as well as the frequent inverse 
                         characteristics of the vertical movements of the latter together 
                         with the structural Alignments of Guapiara and Iva{\'{\i}}.",
            committee = "Vitorello, Icaro (presidente) and Amaral, Gilberto (orientador) 
                         and Amaral, S{\'e}rgio Estanislau do and Coimbra, Armando 
                         M{\'a}rcio and Chiang, Liu Chan",
           copyholder = "SID/SCD",
         englishtitle = "The Ponta Grossa Arch: a proposal for ts configuration and 
                         evolution from the interpretation of remote sensing data",
                label = "55",
             language = "pt",
                pages = "145",
                  ibi = "6qtX3pFwXQZ3r59YD6/GNqRs",
                  url = "http://urlib.net/ibi/6qtX3pFwXQZ3r59YD6/GNqRs",
           targetfile = "publicacao.pdf",
        urlaccessdate = "01 maio 2024"
}