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矿物相律
释义
矿物相律
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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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stable class
stable clustering
stable coherent sheaf
stable cohomology operation
stable cohomotopy group
stable compact leaf
stable composition product
stable condensation
stable convergence
stable coordinate
stable curve
stable difference scheme
stable differentiable mapping
stable differential equation
stable dimension
stable discrete time system
stable discretization
stable distribution
stable element
stable equilibrium
stable equivalence
stable expression
stable fiber bundle
stable flow
stable framing
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