Physico-chemical aspects of recrystalliz
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W. E. Ewers
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Article
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1967
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Springer
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English
โ 517 KB
The driving forces for recrystallization of sulphide minerals that arise from particle size variations (surface energy), from temperature gradients and from the formation of a new phase are compared semi quantitatively. It is shown by expressing these driving forces in terms of gradients in activiti