Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Tolentino Flávio de Oliveira"'
Autor:
Aroldo Misi, Karem Azmy, Alan J. Kaufman, Gustavo Diniz Oliveira, Tolentino Flávio de Oliveira, Andreia Lima Sanches
Publikováno v:
Ore Geology Reviews. 63:76-90
The Vazante Group, as originally described, is a thick marine carbonate-dominated succession adjacent to the Brasilia Fold Belt, on the western border of the Sao Francisco Craton, in south-central Brazil. The sedimentary dolomites of this group conta
Autor:
Marcel Auguste Dardenne, Alan J. Kaufman, Tolentino Flávio de Oliveira, Alcides N. Sial, Karem Azmy, Aroldo Misi
Publikováno v:
Geological Society, London, Memoirs. 36:509-522
The Neoproterozoic successions of the Sao Francisco Craton are primarily represented by the Bambui and Una groups, deposited in cratonic epicontinental basins, and by the Vazante and Vaza Barris/Miaba groups, which accumulated on passive margins on t
Publikováno v:
Precambrian Research. 168:259-270
The Vazante Group consists of a late Mesoproterozoic (∼1.0–1.1 Ga) carbonate-dominated marine platform sequence in east-central Brazil. The upper part of the sequence consists of a glaciomarine diamictite unit overlain by a cap carbonate. The δ1
Publikováno v:
Precambrian Research. 164:160-172
The Vazante Group consists of Precambrian carbonate-dominated platform deposits that extend along more than 300 km in the external zone of the Brasilia Fold Belt of the Sao Francisco Basin in east central Brazil. The sequence is about 4.8 km thick an
Autor:
Lena Virgínia Soares Monteiro, Jorge Silva Bettencourt, Tolentino Flávio de Oliveira, Caetano Juliani
Publikováno v:
Repositório Institucional da USP (Biblioteca Digital da Produção Intelectual)
Universidade de São Paulo (USP)
instacron:USP
Universidade de São Paulo (USP)
instacron:USP
The Vazante Group hosts the Vazante nonsulfide zinc deposit, which comprises high-grade zinc silicate ore (ZnSiO4), and late-diagenetic to epigenetic carbonate-hosted sulfide-rich zinc deposits (e.g. Morro Agudo, Fagundes, and Ambrosia). In the sulfi
Publikováno v:
Precambrian Research. 149:231-248
The Lapa Formation is a thick carbonate sequence (∼900 m) that constitutes the upper part of the Vazante Group on the S˜ Francisco craton, Brazil. It conformably overlies a previously unrecognized glacial diamictite unit of poorly constrained age.
Autor:
Lena Virgínia Soares Monteiro, Jorge Silva Bettencourt, Caetano Juliani, Tolentino Flávio de Oliveira
Publikováno v:
Repositório Institucional da USP (Biblioteca Digital da Produção Intelectual)
Universidade de São Paulo (USP)
instacron:USP
Universidade de São Paulo (USP)
instacron:USP
The Vazante–Paracatu region represents the most important Zn district known in Brazil and includes the Vazante hypogene non-sulfide Zn deposit composed mainly of willemite (Zn2SiO4) and sphalerite-rich carbonate-hosted Zn–(Pb) deposits. Fagundes
Autor:
Carlos Eduardo Silva Coelho, Washington de Jesus Sant'Anna da Franca-Rocha, S. S. Iyer, Ioná de Abreu Cunha, João Batista Guimarães Teixeira, Colombo Celso Gaeta Tassinari, Aroldo Misi, Tolentino Flávio de Oliveira, Adriana S. Rocha Gomes, Valter Mônaco Conceição Filho
Publikováno v:
Repositório Institucional da USP (Biblioteca Digital da Produção Intelectual)
Universidade de São Paulo (USP)
instacron:USP
Universidade de São Paulo (USP)
instacron:USP
The Proterozoic sediment-hosted Zn–(Pb) sulfide and non-sulfide deposits of the Sao Francisco Craton, Brazil, are partially syn-diagenetic and epigenetic and were probably formed during extensional events. The majority of the deposits occur within
Autor:
Marly Babinski, Lena Virgínia Soares Monteiro, A. H. Fetter, Tolentino Flávio de Oliveira, Jorge Silva Bettencourt
Publikováno v:
Repositório Institucional da USP (Biblioteca Digital da Produção Intelectual)
Universidade de São Paulo (USP)
instacron:USP
Universidade de São Paulo (USP)
instacron:USP
The Vazante Group, located in the northwestern part of Minas Gerais, hosts the most important zinc mine in Brazil, the Vazante Mine, which represents a major known example of a hypogene nonsulfide zinc deposit. The main zinc ore is represented by wil
Autor:
Marcel Auguste Dardenne, Ján Veizer, Andreia Lima Sanches, Karem Azmy, Tolentino Flávio de Oliveira, Aroldo Misi
Publikováno v:
Precambrian Research. 112:303-329
The Vazante Formation consists of approximately 1700 m of mainly microbial mats and stromatolitic reefal lenses that were deposited on shallow marine platform and have been entirely dolomitized. Samples representing different dolomite generations wer