The difference between Pau-a-Pique gold deposit (Mato Grosso State) and classic gold deposits are hosted in conglomerates

Diferenças Entre os Depósitos Auríferos do Grupo Aguapei (Estado de Mato Grosso) e os Clássicos Exemplos de Ouro em Conglomerados

dc.contributoren-US
dc.contributorpt-BR
dc.creatorFERNANDES, CARLOS JOSÉ
dc.creatorPULZ, GÊNOVA MARIA
dc.creatorKUYUMJIAN, RAUL MINAS
dc.creatorPINHO, FRANCISCO EGÍDIO CAVALCANTE
dc.date2005-06-30
dc.date.accessioned2018-11-07T21:59:17Z
dc.date.available2018-11-07T21:59:17Z
dc.identifierhttps://seer.ufrgs.br/PesquisasemGeociencias/article/view/19534
dc.identifier10.22456/1807-9806.19534
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/2192306
dc.descriptionGold prospects in the Aguapeí Folded Belt are situated in the southwestern portion of the Amazon Craton, within the Alto Guaporé Province, southwestern state of Mato Grosso. The mineralizations are mainly concentrated in the Pau-a-Pique Deposit (south), Lavrinha Region (central), and São Vicente Mine (north). Gold ore comprises quartz veins and disseminations in the low-grade metamorphic metassedimentary rocks from the Aguapeí Group. This stratigraphic unit was strongly deformed by the Sunsás-Aguapeí Orogeny (1.28-0.95 Ga). The Aguapeí gold deposits differ in their petrography, chemistry, structural aspects and age from world classic gold deposits associated with coarse clastic sedimentary sequences (Witwatersrand, Jacobina, Tarkwa, etc.). This study discusses the main differences between Aguapeí gold deposits and the classic worldwide deposits hosted by conglomeratesen-US
dc.descriptionGold prospects in the Aguapeí Folded Belt are situated in the southwestern portion of the Amazon Craton, within the Alto Guaporé Province, southwestern state of Mato Grosso. The mineralizations are mainly concentrated in the Pau-a-Pique Deposit (south), Lavrinha Region (central), and São Vicente Mine (north). Gold ore comprises quartz veins and disseminations in the low-grade metamorphic metassedimentary rocks from the Aguapeí Group. This stratigraphic unit was strongly deformed by the Sunsás-Aguapeí Orogeny (1.28-0.95 Ga). The Aguapeí gold deposits differ in their petrography, chemistry, structural aspects and age from world classic gold deposits associated with coarse clastic sedimentary sequences (Witwatersrand, Jacobina, Tarkwa, etc.). This study discusses the main differences between Aguapeí gold deposits and the classic worldwide deposits hosted by conglomerates.pt-BR
dc.formatapplication/pdf
dc.languagepor
dc.publisherInstituto de Geociências /Universidade Federal do Rio Grande do Sulpt-BR
dc.relationhttps://seer.ufrgs.br/PesquisasemGeociencias/article/view/19534/pdf
dc.sourcePesquisas em Geociências; v. 32, n. 1 (2005): Pesquisas em Geociências; 17-26pt-BR
dc.source1807-9806
dc.source1518-2398
dc.subjecten-US
dc.subjectconglomerate, gold deposits, Aguapeí Groupen-US
dc.subjectGeociências;Geologia;Geografia;Geodésia;Paleontologia;Engenharia Cartográficapt-BR
dc.subjectconglomerate; gold deposits; Aguapeí Group.pt-BR
dc.subjectGeociênciaspt-BR
dc.titleThe difference between Pau-a-Pique gold deposit (Mato Grosso State) and classic gold deposits are hosted in conglomeratesen-US
dc.titleDiferenças Entre os Depósitos Auríferos do Grupo Aguapei (Estado de Mato Grosso) e os Clássicos Exemplos de Ouro em Conglomeradospt-BR
dc.typeArtículos de revistas
dc.typeArtículos de revistas
dc.coverageMato Grosso;Brasilpt-BR
dc.coveragept-BR
dc.coveragept-BR


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