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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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topological isotopy
topological kernel
topological knot
topological K-theory
topological lattice
topological limit
topological linear space
topological logic
topologically algebraic
topologically complete set
topologically complete space
topologically conjugate
topologically conjugate homeomorphism
topologically embeddable
topologically equivalent
topologically equivalent spaces
topologically free set
topologically hyperbolic manifold
topologically inequivalent
topologically invariant
topologically irreducible representation
topologically isomorphic
topologically isotopic embedding
topologically nilpotent element
topologically ringed space
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