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dc.contributor.authorSeimetz, Eduardo Xavier-
dc.contributor.authorCosta, Alexandre Santos Jeronimo da-
dc.contributor.authorBorges, Welitom Rodrigues-
dc.contributor.authorIanniruberto, Marco-
dc.contributor.authorCanata, Rafael Espindola-
dc.date.accessioned2023-10-27T12:48:43Z-
dc.date.available2023-10-27T12:48:43Z-
dc.date.issued2023-01-31-
dc.identifier.citationSEIMETZ, Eduardo Xavier et al. Geoelectric signature of gold mineralization in the Alta Floresta Gold Province, Mato Grosso State, Brazil. Minerals, [S.l.], v. 13, n. 2, 203, 2023. DOI: https://doi.org/10.3390/min13020203. Disponível em: https://www.mdpi.com/2075-163X/13/2/203. Acesso em: 27 out. 2023.pt_BR
dc.identifier.urihttp://repositorio2.unb.br/jspui/handle/10482/46753-
dc.language.isoengpt_BR
dc.publisherMDPIpt_BR
dc.rightsAcesso Abertopt_BR
dc.titleGeoelectric signature of gold mineralization in the Alta Floresta Gold Province, Mato Grosso State, Brazilpt_BR
dc.typeArtigopt_BR
dc.subject.keywordPolarização induzidapt_BR
dc.subject.keywordProvíncia Aurífera de Alta Florestapt_BR
dc.subject.keywordOuro - minas e mineraçãopt_BR
dc.rights.licenseCopyright: © 2023 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https:// creativecommons.org/licenses/by/ 4.0/).pt_BR
dc.identifier.doihttps://doi.org/10.3390/min13020203pt_BR
dc.description.abstract1The Alta Floresta Gold Province (PAAF) is abundant in gold deposits and, located in the state of Mato Grosso, Brazil, is an ideal place to study the geoelectric signature of gold mineralization. Auriferous mineralization occurs along shear zones in quartz veins and disseminated granites in this region. Ores are associated with oxides and sulfides, mainly with pyrites. To identify primary gold or continuities of the mineralized zones, data were acquired using the geophysical methods of electrical resistivity and induced polarization in three gold mines: Raimunda, Truilio, and Porteira. Dipole–dipole arrays with electrode spacings of 20 and 25 m were used to investigate up to 100 m in depth. Resistivity and chargeability range scales were developed with statistical analyses of all the geophysical and geological data. The geophysical models of the Raimunda and Truilio gold mines showed coherence with the boreholes, but the geophysical models of the Porteira gold mine were not coherent with the boreholes. The resistivity and chargeability parameters indicated that the lithotypes (soils, saprolites, and monzogranites) could be characterized and identified as potential mineralized targets. The soils ranged from 1000 to 8000 ohm.m, the saprolites had values from 150 to 800 ohm.m, and the monzogranite values were from 1100 to 9000 ohm.m. The mineralized targets had values from 18 to 35 mV/V. The results confirm the efficiency of the resistivity and induced polarization methods to find sulfides in shear zones in the Alta Floresta Gold Province.pt_BR
dc.identifier.orcidhttps://orcid.org/0000-0001-5726-5884pt_BR
dc.identifier.orcidhttps://orcid.org/0000-0002-5158-1947pt_BR
dc.identifier.orcidhttps://orcid.org/0000-0002-9056-9668pt_BR
dc.contributor.affiliationUniversity of Brasilia, Institute of Geosciencespt_BR
dc.contributor.affiliationUniversity of Brasilia, Institute of Geosciencespt_BR
dc.contributor.affiliationUniversity of Brasilia, Institute of Geosciencespt_BR
dc.contributor.affiliationUniversity of Brasilia, Institute of Geosciencespt_BR
dc.contributor.affiliationFederal University of Paraná, Institute of Geology, Earth Science Sectorpt_BR
dc.description.unidadeInstituto de Geociências (IG)pt_BR
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