2005
DOI: 10.2113/100.1.0007
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Geology and SHRIMP U-Pb Geochronology of the Igarape Bahia Deposit, Carajas Copper-Gold Belt, Brazil: An Archean (2.57 Ga) Example of Iron-Oxide Cu-Au-(U-REE) Mineralization

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Cited by 128 publications
(74 citation statements)
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“…The CMP is part of the Archean tectonic domain known as the Itacaiúnas Shear Belt, found in the eastern portion of the Amazonian craton, which is composed of high-grade metamorphic complexes, volcanic-sedimentary sequences, and granite-greenstone terrains [14]. The Carajá s Belt is a highly mineralized province, with enormous reserves of iron and manganese, as well as Au-Cu deposits encompassing the Carajá s gold-copper belt [15]. The N1 area has rocks of the Grã o Pará Group, and has been subdivided into two units: volcanic rocks of the Parauapebas Formation [16], and the ironstones of the Carajá s Formation [17].…”
Section: Study Areamentioning
confidence: 99%
“…The CMP is part of the Archean tectonic domain known as the Itacaiúnas Shear Belt, found in the eastern portion of the Amazonian craton, which is composed of high-grade metamorphic complexes, volcanic-sedimentary sequences, and granite-greenstone terrains [14]. The Carajá s Belt is a highly mineralized province, with enormous reserves of iron and manganese, as well as Au-Cu deposits encompassing the Carajá s gold-copper belt [15]. The N1 area has rocks of the Grã o Pará Group, and has been subdivided into two units: volcanic rocks of the Parauapebas Formation [16], and the ironstones of the Carajá s Formation [17].…”
Section: Study Areamentioning
confidence: 99%
“…In the latter, SHRIMP zircon ages of 3,002 ± 14 Ma and 2,861 ± 12 Ma are considered as representative of the parent magmatic rock and the granulite facies metamorphism, respectively (Pidgeon et al 2000). The basement rocks are overlain by meta-volcanic-sedimentary units of the Rio Novo Group (Hirata et al 1982) and the 2.73-2.76 Ga Itacaiúnas Supergroup (Igarapé Salobo, Igarapé Pojuca, Grão Pará, and Igarapé Bahia groups; Wirth et al 1986;Docegeo 1988;Machado et al 1991;Trendall et al 1998;Krymsky et al 2002;Galarza et al 2003;Pimentel et al 2003;Tallarico et al 2005). These volcanic-sedimentary sequences comprise variably deformed and metamorphosed (low greenshist to amphibolite facies) basic and felsic volcanic and pyroclastic rocks, iron formations, and clastic sedimentary rocks (Wirth et al 1986;Hirata et al 1982;Docegeo 1988;Machado et al 1991).…”
Section: Regional Geology Of the Carajas Mineral Provincementioning
confidence: 99%
“…Approximately 140 t of gold have been produced from the supergene-enriched zone, which is now practically exhausted. Both syngenetic (Ferreira Filho, 1985;Althoff et al, 1994;Almada and Villas, 1999;Dreher andXavier, 2001, 2005) and epigenetic (Huhn and Nascimento, 1997;Tallarico et al, 1998Tallarico et al, , 2000Tallarico et al, , 2005Oliveira et al, 1998;Lindenmayer et al, 1998;Tazava, 1999) models have been proposed for the Igarapé Bahia mineralization. In addition, some epigeneticists postulate a genetic link of the mineralization with Paleoproterozoic granitic magmatism (Lindenmayer et al, 1998;Tallarico et al, 2000).…”
Section: Introductionmentioning
confidence: 99%