ASSINATURAS GEOQUIMICAS DE SEDIMENTOS DE CORRENTE DOS TERRENOS PRECAMBRIANOS DO URUGUAY
| Main Author: | |
|---|---|
| Publication Date: | 2022 |
| Format: | Article |
| Language: | eng |
| Source: | Geochimica Brasiliensis (Online) |
| Download full: | https://geobrasiliensis.org.br/geobrasiliensis/article/view/696 |
Summary: | Geochemical data of Uruguayan crystalline terrains collected in the 80’s were recovery by the National Mining and Geology Directorate of Uruguay (DINAMIGE) in 2020 involving 32,000 soil and stream sediment samples analyzed for 22 elements (Ag, As, B, Ba, Be, Cd, Co, Cr, Cu, Fe, Mn, Mo, Nb, Ni, P, Pb, Sb, Sn, V, W, Y and Zn) by direct current plasma spectrometry. A set of 6755 samples of these data, more or less 21% of the total, were processed by multivariate statistical methods and geographic information system (GIS) procedures in this study aiming characterization of geochemical signatures derived from environmental and geological processes. Samples were classified as background, anomalies and outliers at the beginning, so geology classification with GIS and discriminant analysis allowed to define 14 signatures related to lithologies, hidrotermalism, sulphide occurrence, superficial or mixed processes. 84.4% of samples were considered background associated to the geological units, 8.9% of samples were undefined outliers, 2.6% of samples were interpreted as lithological anomalies, 3.8% of samples were associated to hidrothermalism, superficial processes or mixed models and only 0.3% of the samples were probably related to sulphide deposits occurrences. |
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ASSINATURAS GEOQUIMICAS DE SEDIMENTOS DE CORRENTE DOS TERRENOS PRECAMBRIANOS DO URUGUAYAnomaly, background, environment, exploration, outliers, trace-elementsGeochemical data of Uruguayan crystalline terrains collected in the 80’s were recovery by the National Mining and Geology Directorate of Uruguay (DINAMIGE) in 2020 involving 32,000 soil and stream sediment samples analyzed for 22 elements (Ag, As, B, Ba, Be, Cd, Co, Cr, Cu, Fe, Mn, Mo, Nb, Ni, P, Pb, Sb, Sn, V, W, Y and Zn) by direct current plasma spectrometry. A set of 6755 samples of these data, more or less 21% of the total, were processed by multivariate statistical methods and geographic information system (GIS) procedures in this study aiming characterization of geochemical signatures derived from environmental and geological processes. Samples were classified as background, anomalies and outliers at the beginning, so geology classification with GIS and discriminant analysis allowed to define 14 signatures related to lithologies, hidrotermalism, sulphide occurrence, superficial or mixed processes. 84.4% of samples were considered background associated to the geological units, 8.9% of samples were undefined outliers, 2.6% of samples were interpreted as lithological anomalies, 3.8% of samples were associated to hidrothermalism, superficial processes or mixed models and only 0.3% of the samples were probably related to sulphide deposits occurrences.Dados geoquímicos do cristalino Uruguaio coletados nos 80’s foram recuperados pela Direção Nacional de Mineração e Geologia do Uruguai (DINAMIGE) em 2020 considerando 32.000 amostras de solos e sedimentos de corrente analisadas para 22 elementos químicos (Ag, As, B, Ba, Be, Cd, Co, Cr, Cu, Fe, Mn, Mo, Nb, Ni, P, Pb, Sb, Sn, V, W, Y and Zn) por meio de espectrometria de plasma de corrente direta. Uma parte de essos datos, de 6755 amostras, ou seja, aproximadamente 21% do total, foram processadas por métodos estatísticos multivariados e procedimentos de sistemas de informação geográfica (GIS) objetivando a caracterização das anomalias geoquímicas derivadas de processos ambientais e geológicos. As amostras foram inicialmente classificadas como relacionadas ao teor de fundo, anomalias ou “outliers” e posteriormente, considerando a geologia associada a cada amostra e análise discriminante definiram-se 14 assinaturas geoquímicas relacionadas com litologias, hidrotermalismo, ocorrência de depósitos de sulfetos, processos superficiais ou mixturados. 84,4% das amostras foram consideradas como teor de fondo relacionado com as formações geológicas, 8,9% foram “outliers”, 2,6% consideraram-se anomalias litológicas, 3,8% sugeriram envolvimento com processos hidrotermais, superficiais ou mixturados e finalmente 0,3% das amostras relacionaram-se possivelmente com depósitos de sulfetos.Sociedade Brasileira de Geoquímica2022-04-05info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://geobrasiliensis.org.br/geobrasiliensis/article/view/69610.21715/GB2358-2812.202236004Geochimica Brasiliensis; Vol. 36 (2022): Continuous Publication; e-22004Geochimica Brasiliensis; Vol. 36 (2022): Continuous Publication; e-22004Geochimica Brasiliensis; v. 36 (2022): Continuous Publication; e-220042358-28120102-9800reponame:Geochimica Brasiliensis (Online)instname:Sociedade Brasileira de Geoquímica (SBGq)instacron:SBGQenghttps://geobrasiliensis.org.br/geobrasiliensis/article/view/696/714Copyright (c) 2022 Geochimica Brasiliensisinfo:eu-repo/semantics/openAccessAlba, Jose Maria Filippini2023-06-03T12:16:32Zoai:ojs.geobrasiliensis.org.br:article/696Revistahttps://brjg.sbgf.org.brONGhttps://geobrasiliensis.org.br/geobrasiliensis/oaigeobrasilliensis@gmail.com | jorge.dilena@gmail.com2358-28120102-9800opendoar:2023-06-03T12:16:32Geochimica Brasiliensis (Online) - Sociedade Brasileira de Geoquímica (SBGq)false |
| dc.title.none.fl_str_mv |
ASSINATURAS GEOQUIMICAS DE SEDIMENTOS DE CORRENTE DOS TERRENOS PRECAMBRIANOS DO URUGUAY |
| title |
ASSINATURAS GEOQUIMICAS DE SEDIMENTOS DE CORRENTE DOS TERRENOS PRECAMBRIANOS DO URUGUAY |
| spellingShingle |
ASSINATURAS GEOQUIMICAS DE SEDIMENTOS DE CORRENTE DOS TERRENOS PRECAMBRIANOS DO URUGUAY Alba, Jose Maria Filippini Anomaly, background, environment, exploration, outliers, trace-elements |
| title_short |
ASSINATURAS GEOQUIMICAS DE SEDIMENTOS DE CORRENTE DOS TERRENOS PRECAMBRIANOS DO URUGUAY |
| title_full |
ASSINATURAS GEOQUIMICAS DE SEDIMENTOS DE CORRENTE DOS TERRENOS PRECAMBRIANOS DO URUGUAY |
| title_fullStr |
ASSINATURAS GEOQUIMICAS DE SEDIMENTOS DE CORRENTE DOS TERRENOS PRECAMBRIANOS DO URUGUAY |
| title_full_unstemmed |
ASSINATURAS GEOQUIMICAS DE SEDIMENTOS DE CORRENTE DOS TERRENOS PRECAMBRIANOS DO URUGUAY |
| title_sort |
ASSINATURAS GEOQUIMICAS DE SEDIMENTOS DE CORRENTE DOS TERRENOS PRECAMBRIANOS DO URUGUAY |
| author |
Alba, Jose Maria Filippini |
| author_facet |
Alba, Jose Maria Filippini |
| author_role |
author |
| dc.contributor.author.fl_str_mv |
Alba, Jose Maria Filippini |
| dc.subject.por.fl_str_mv |
Anomaly, background, environment, exploration, outliers, trace-elements |
| topic |
Anomaly, background, environment, exploration, outliers, trace-elements |
| description |
Geochemical data of Uruguayan crystalline terrains collected in the 80’s were recovery by the National Mining and Geology Directorate of Uruguay (DINAMIGE) in 2020 involving 32,000 soil and stream sediment samples analyzed for 22 elements (Ag, As, B, Ba, Be, Cd, Co, Cr, Cu, Fe, Mn, Mo, Nb, Ni, P, Pb, Sb, Sn, V, W, Y and Zn) by direct current plasma spectrometry. A set of 6755 samples of these data, more or less 21% of the total, were processed by multivariate statistical methods and geographic information system (GIS) procedures in this study aiming characterization of geochemical signatures derived from environmental and geological processes. Samples were classified as background, anomalies and outliers at the beginning, so geology classification with GIS and discriminant analysis allowed to define 14 signatures related to lithologies, hidrotermalism, sulphide occurrence, superficial or mixed processes. 84.4% of samples were considered background associated to the geological units, 8.9% of samples were undefined outliers, 2.6% of samples were interpreted as lithological anomalies, 3.8% of samples were associated to hidrothermalism, superficial processes or mixed models and only 0.3% of the samples were probably related to sulphide deposits occurrences. |
| publishDate |
2022 |
| dc.date.none.fl_str_mv |
2022-04-05 |
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info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion |
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article |
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publishedVersion |
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https://geobrasiliensis.org.br/geobrasiliensis/article/view/696 10.21715/GB2358-2812.202236004 |
| url |
https://geobrasiliensis.org.br/geobrasiliensis/article/view/696 |
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10.21715/GB2358-2812.202236004 |
| dc.language.iso.fl_str_mv |
eng |
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eng |
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https://geobrasiliensis.org.br/geobrasiliensis/article/view/696/714 |
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Copyright (c) 2022 Geochimica Brasiliensis info:eu-repo/semantics/openAccess |
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Copyright (c) 2022 Geochimica Brasiliensis |
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openAccess |
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application/pdf |
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Sociedade Brasileira de Geoquímica |
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Sociedade Brasileira de Geoquímica |
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Geochimica Brasiliensis; Vol. 36 (2022): Continuous Publication; e-22004 Geochimica Brasiliensis; Vol. 36 (2022): Continuous Publication; e-22004 Geochimica Brasiliensis; v. 36 (2022): Continuous Publication; e-22004 2358-2812 0102-9800 reponame:Geochimica Brasiliensis (Online) instname:Sociedade Brasileira de Geoquímica (SBGq) instacron:SBGQ |
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Sociedade Brasileira de Geoquímica (SBGq) |
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SBGQ |
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SBGQ |
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Geochimica Brasiliensis (Online) |
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Geochimica Brasiliensis (Online) |
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Geochimica Brasiliensis (Online) - Sociedade Brasileira de Geoquímica (SBGq) |
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geobrasilliensis@gmail.com | jorge.dilena@gmail.com |
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