Abstract
Natural iron-bearing rutile, formed under low temperature hydrothermal conditions, is chemically homogeneous on an electron-microscope scale (at a resolution of about 10 Å). On annealing at temperatures between 475° and 600° C precipitation of an iron-rich phase occurs. The precipitation sequence involves two transitional stages before the formation of hematite, the equilibrium precipitate. The first phase is coherent with the rutile structure and has the general characteristics of Guinier-Preston zones. The second transitional phase is a monoclinic variant of the rutile structure and is partially coherent with the matrix. Annealing experiments enable a Time-Temperature-Transformation (TTT) plot to be constructed for the exsolution process and the kinetics are interpreted in terms of the structural changes involved at each stage of the process.
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Putnis, A. The mechanism of exsolution of hematite from iron-bearing rutile. Phys Chem Minerals 3, 183–197 (1978). https://doi.org/10.1007/BF00308121
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DOI: https://doi.org/10.1007/BF00308121