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Restrições à Petrogénese do Talco Ore no Sudoeste do Montana

Restrições à Petrogénese do Talco Ore no Sudoeste do Montana

          
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About the Book

Talco, um filossilicato de magnésio, é utilizado em muitos produtos, incluindo tintas, borracha, cerâmica, cosméticos, e plásticos. A mineralização do talco ocorre geralmente em condições metamórficas de baixo grau e requer uma fonte significativa de magnésio. Processos de formação, tais como metamorfismo ou eventos hidrotermais, dos corpos de talco, controlam as composições inerentes e podem ditar que impurezas estão presentes. Este estudo centra-se num depósito de talco próximo de Alder, Montana, um de uma série de depósitos pré-cambrianos de alta pureza dentro desta região. Os resultados petrográficos indicam que o mármore dolomítico foi substituído pseudomorficamente por talco. Isto implica que foi fornecido magnésio suficiente da rocha hospedeira e sílica pelo fluido hidrotermais. As amostras de talco relativamente puro (>90% por XRD) têm apenas vestígios de Al, Ca, e K, e são muito baixas em elementos de terras raras (REE). Os lixiviados ácidos acéticos de unidades ricas em carbonatos produzem padrões de REE leves enriquecidos e concentrações de REE mais elevadas do que as amostras de talco puro. Os padrões e concentrações de elementos de terras raras sugerem que o talco herdou os seus REE do carbonato durante a recristalização do carbonato para o talco.


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Product Details
  • ISBN-13: 9786205331415
  • Publisher: KS Omniscriptum Publishing
  • Publisher Imprint: Edicoes Nosso Conhecimento
  • Height: 229 mm
  • No of Pages: 64
  • Spine Width: 4 mm
  • Width: 152 mm
  • ISBN-10: 6205331411
  • Publisher Date: 07 Nov 2022
  • Binding: Paperback
  • Language: Portuguese
  • Returnable: N
  • Weight: 104 gr


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Restrições à Petrogénese do Talco Ore no Sudoeste do Montana
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