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Goldschmidt's mineralogical phase rule |
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Goldschmidt's mineralogical phase rule [′gōl‚shmits ‚min·ə·rə′läj·ə·kəl ¦fāz ‚rül]
(geology) The rule that the probability of finding a system with degrees of freedom less than two is small under natural rock-forming conditions. Want to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit the webmaster's page for free fun content. |
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