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dc.contributor.authorSommer, Jussara Alves Pinheiropt_BR
dc.contributor.authorLima, Evandro Fernandes dept_BR
dc.contributor.authorSaldanha, Dejanira Luderitzpt_BR
dc.contributor.authorSommer, Carlos Augustopt_BR
dc.contributor.authorPierosan, Ronaldopt_BR
dc.date.accessioned2010-05-20T04:16:26Zpt_BR
dc.date.issued2006pt_BR
dc.identifier.issn1518-2398pt_BR
dc.identifier.urihttp://hdl.handle.net/10183/22625pt_BR
dc.description.abstractThe remote sensing products which are generated by orbitals sensors of middle spatial and spectral resolution and the development of new technique of digital image processing has been a auxiliary tool in the basic geological surveys. In this work was utilized images obtained from the ASTER sensor (Advanced Spaceborne Thermal Emission and Reflection Radiometer) to identify the lithologies in the Ramada Plateau area, situated closed to Vila Nova do Sul town, in the southernmost Brazil, giving emphasis to the volcanic sequence of the plateau and the encase sedimentary rocks unit. The volcanic unit represent a important part of the Neoproterozoic alkaline magmatism in the Sul-rio-grandense Shield and is interpreted as one of the volcanic cycles of the post-collisional period of Brasiliano Cycle in the southern Brazil. The selective principal component analysis technique was used in the digital image processing, because it provided the best results enhancing the existent spectral differences of the studied lithologies. In this processing were utilized only two spectral bands to reduce the data dimensionality, permitting a better interpretation of them. The first generated image (PC1) concentrate the common information of the two bands (albedo and topographic shading), while PC2 image present the differential information of the scene, representing the spectral contrast of the two original bands. From this technique was generated a color composite image from the PC’s2 images of the pair of bands 4-5 (R), 3-4 (G) and 8-9 (B). This image has shown the spectral differences between volcanic rocks of the Ramada Plateau and the sedimentary rocks of the Maricá Group and its individualization in two sub-units, mainly considering the concentration of rhyolitic dykes and sills in the north of the area. In this study was identify too in the southwestern portion of the Ramada Plateau, a dioritic intrusive body.en
dc.format.mimetypeapplication/pdf
dc.language.isoporpt_BR
dc.relation.ispartofPesquisas em Geociências. Vol. 33, n. 1 (2006), p. 23-36pt_BR
dc.rightsOpen Accessen
dc.subjectSensoriamento remotopt_BR
dc.subjectRemote sensingen
dc.subjectGeological mappingen
dc.subjectMapeamento geológico : Rochas vulcânicaspt_BR
dc.subjectVila Nova do Sul (RS)pt_BR
dc.subjectVolcanic rocksen
dc.subjectPrincipal componentsen
dc.titleO uso de imagens do Sensor Aster no mapeamento de unidades vulcano-sedimentares do Platô da Ramada, Vila Nova do Sul, RSpt_BR
dc.typeArtigo de periódicopt_BR
dc.identifier.nrb000603238pt_BR
dc.type.originNacionalpt_BR


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