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mineralogical phase rule
释义
mineralogical phase rule
Encyclopedia
理学
吉布斯相律
释
mineralogical phase rule
矿物相律
反映变质岩形成过程中达到热力学多相平衡时,矿物相数与独立组分数之间关系的法则。是吉布斯相律在封闭体系中的应用。由挪威科学家V.M.戈尔德施密特根据吉布斯相律于1911年提出,又称戈尔德施密特矿物相律。
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reporting offences by use of anonymous boxes
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report of reading for examination
report of regional geological survey
report of risk assessment
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Report on China City Development
report on execution submitted to the emperor for review
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repository of the Qing Historiographer's office
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更新时间:2026/10/29 17:06:46