An experimental investigation of the system MgO-SiO 2 -H 2 O-CO 2

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ID: 293036
1969
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Abstract
Equilibrium reactions of this system were experimentally investigated at pressures to 7000 bars and temperatures to 660 degrees C. Serpentine can coexist only with a CO ~2~ -poor fluid, and the lower stability limits of forsterite and talc are determined; talc is a metamorphic mineral at high pressures. The upper and lower stability limits of talc + magnesite are also determined and set limits on the temperature of formation of talc-bearing magnesite deposits and magnesite-bearing talc deposits. The conditions of origin for a number of types and specific localities of magnesite deposits are discussed in the light of these experimental studies.
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openalex_W2029564307 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors Wilhelm Johannes
Journal american journal of science
Year 1969
DOI
10.2475/ajs.267.9.1083
URL
https://ajs.scholasticahq.com/article/59360.pdf
Keywords Keywords not found

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