Metadolomitos talcificados do Grupo Itaiacoca, Paraná: regime de fluidos e implicações genéticas

@inproceedings{Saunite2011MetadolomitosTD,
  title={Metadolomitos talcificados do Grupo Itaiacoca, Paran{\'a}: regime de fluidos e implicaç{\~o}es gen{\'e}ticas},
  author={Danilo Marques Saunite and R. Bello and F{\'a}bio Ramos Dias de Andrade and G. Szab{\'o}},
  year={2011}
}
Brazil's largest talc deposits occur in the Itaiacoca Group, which is a low-grade metasedimentary belt composed mainly of dolomitic rocks. Fluid inclusions from three geological settings in which talc was formed differently were analysed. Talc schist ore occur along transcurrent shear zones. These talc schists are host to quartz veins, which indicates prolonged circulation of hydrothermal fluids at high water:rock ratios. The fluid inclusions in the quartz veins contain predominantly low… Expand

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