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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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surface of least area
surface of Liouville type
surface of materials
surface of negative curvature
surface of order n
Surface of phase change heat transfer
surface of positive curvature
surface of r contours
surface of revolution
surface-of-revolution parallel
surface of rotation
surface of screw motion
surface of second order
surface of section
surface of semiconductor
surface of singularities
surface of slope
surface of spatial type
surface of striction
surface of the second class
surface of third order
surface of translation
surface of zero velocity
surface optics
surface order
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