ASSINATURAS GEOQUIMICAS DE SEDIMENTOS DE CORRENTE DOS TERRENOS PRECAMBRIANOS DO URUGUAY

Bibliographic Details
Main Author: Alba, Jose Maria Filippini
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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spelling 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
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv https://geobrasiliensis.org.br/geobrasiliensis/article/view/696
10.21715/GB2358-2812.202236004
url https://geobrasiliensis.org.br/geobrasiliensis/article/view/696
identifier_str_mv 10.21715/GB2358-2812.202236004
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv https://geobrasiliensis.org.br/geobrasiliensis/article/view/696/714
dc.rights.driver.fl_str_mv Copyright (c) 2022 Geochimica Brasiliensis
info:eu-repo/semantics/openAccess
rights_invalid_str_mv Copyright (c) 2022 Geochimica Brasiliensis
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Sociedade Brasileira de Geoquímica
publisher.none.fl_str_mv Sociedade Brasileira de Geoquímica
dc.source.none.fl_str_mv 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
instname_str Sociedade Brasileira de Geoquímica (SBGq)
instacron_str SBGQ
institution SBGQ
reponame_str Geochimica Brasiliensis (Online)
collection Geochimica Brasiliensis (Online)
repository.name.fl_str_mv Geochimica Brasiliensis (Online) - Sociedade Brasileira de Geoquímica (SBGq)
repository.mail.fl_str_mv geobrasilliensis@gmail.com | jorge.dilena@gmail.com
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