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Mineral equilibria in the MgO-SiO 2 -H 2 O system; I, Talc-chrysotile-forsterite-brucite stability relations

  • Hemley J
  • Montoya J
  • Christ C
  • et al.
American Journal of Science (1977) 277(3) 322-351
DOI: 10.2475/ajs.277.3.322
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Abstract

The silica-dependent mineral equilibria in the system MgO-SiO2-H2O for reactions talc + 5H2O = chrysotile + 2H4SiO4 and talc + 4H2O = 1.5 forsterite + 2.5H4SiO4 were investigated from 200° to 600°C at 1kb H2O and at 90°C and 1 bar total pressure.

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APA

Hemley, J. J., Montoya, J. W., Christ, C. L., & Hostetler, P. B. (1977). Mineral equilibria in the MgO-SiO 2 -H 2 O system; I, Talc-chrysotile-forsterite-brucite stability relations. American Journal of Science, 277(3), 322–351. https://doi.org/10.2475/ajs.277.3.322

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