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矿物相律
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矿物相律
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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on-link care-of address, LCoA
On Literary Writers in Modern China
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Only by Ideals and Disciplines Can We Unite Together
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