Use este identificador para citar ou linkar para este item: https://rigeo.sgb.gov.br/handle/doc/25386
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dc.contributor.authorSILVA, Adolfo Barbosa da-
dc.contributor.authorSILVA, Marcelo Ferreira da-
dc.contributor.authorREIMOLD, Wolf Uwe-
dc.contributor.authorALVES, Felipe da Mota-
dc.contributor.authorLAGO, Alexandre Lisboa-
dc.contributor.authorCOUTO JR, Marco Antônio-
dc.contributor.authorFRASCA, Antônio Augusto S.-
dc.contributor.authorRIBEIRO, Pedro Sérgio Estevam-
dc.date.accessioned2025-01-13T18:58:47Z-
dc.date.available2025-01-13T18:58:47Z-
dc.date.issued2024-
dc.identifier.citationSILVA, Adolfo Barbosa da; SILVA, Marcelo Ferreira da; REIMOLD, Wolf Uwe; ALVES, Felipe da Mota; LAGO, Alexandre Lisboa; COUTO JR, Marco Antônio; FRASCA, Antônio Augusto S.; RIBEIRO, Pedro Sérgio Estevam. The aerogeophysical atlas of Tocantins state: synthesis of magnetic anomaly and radioelement maps with emphasys on regional signatures and the Serra da Cangalha impact structure. Brazilian Journal of Geophysics, Rio de Janeiro, v. 42, n. 2, p. 1-10, 2024. DOI: http://doi.org/10.22564/brjg.v42i2.2316.pt_BR
dc.identifier.issn2764-8044-
dc.identifier.urihttps://rigeo.sgb.gov.br/handle/doc/25386-
dc.description.abstractThe Tocantins State Aerogeophysical Atlas (TSAA) is an institutional product of the Geological Survey of Brazil. It is aimed at promoting the use of airborne magnetic and gamma-ray spectrometry data to support geophysical and geological research at state level. Here, we present a synthesis of the TSAA with special emphasis on the interpretation of the magnetic (Anomalous Magnetic Field, First Vertical Derivative (FVD), and Total Gradient Amplitude (TGA) images) and radiometric (RGB composite color map of concentrations, Inverse Images of K, eTh, and eU, and Normalized eU enhancement) map. In particular, the radiometric data for the Serra da Cangalha impact structure in northeast Tocantins are discussed. For Tocantins State, the results show that the radiometric and/or magnetic signatures of geological units (e.g., Mosquito Formation basalts; granite-gneiss/migmatite terrains) and structural features (e.g., dykes and lineaments), or related exogenous deposits (Serra Geral do Tocantins quartzose soils; alluvial deposits of main drainage channels) can be visualized well on regional-scale maps. Analysis of radiometric ratios for the area of the Serra da Cangalha impact structure indicates that eU concentrations are enriched in the annular basin around the central uplift structure, and in the zone straddling the contact between the Piauí and Pedra de Fogo formations. In the latter case, the elevated eU concentrations could be related to brecciated chert layers or silicified sandstones.pt_BR
dc.language.isoenpt_BR
dc.publisherSociedade Brasileira de Geofísicapt_BR
dc.rightsopenpt_BR
dc.subjectMAGNETOMETRIApt_BR
dc.subjectESPECTROMETRIA DE RAIOS GAMApt_BR
dc.subjectESPECTROMETRIA GAMApt_BR
dc.subjectINTEGRAÇÃO GEOLÓGICO-GEOFÍSICApt_BR
dc.subjectSERRA DA CANGALHApt_BR
dc.subjectTOCANTINSpt_BR
dc.titleThe aerogeophysical atlas of Tocantins state: synthesis of magnetic anomaly and radioelement maps with emphasys on regional signatures and the Serra da Cangalha impact structurept_BR
dc.typeArticlept_BR
dc.localRio de Janeiropt_BR
dc.creator.affilliationUniversidade de Brasíliapt_BR
dc.creator.affilliationVale S/Apt_BR
dc.identifier.doihttp://doi.org/10.22564/brjg.v42i2.2316-
dc.subject.enMAGNETOMETRYpt_BR
dc.subject.enGAMMA-RAY SPECTROMETRYpt_BR
dc.subject.enGEOLOGICAL-GEOPHYSICAL INTEGRATIONpt_BR
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