是一种介于变质作用和典型的岩浆作用之间的一种有不同性质流体参加的造岩作用和成矿作用引的总称。
从动力学系统分析，区域变质作用混合岩化作用变质深熔作用是温压递进性变质作用。
According to the systematic kinetic analysis the processes from regional metamorphisms to migmatizations to metamorphic anatexis are the temperature-pressure progressive metamorphic processes.
有关混合岩及混合岩化作用形成机理的不同认识，至今在地质学和岩石学中仍是一个争论问题。
Migmatite and mechanism of migmatization have been controversial issues in the study of geology and petrology for the past so years.
白云岩成因的研究目前还处于假说阶段，主要包括蒸发、渗透回流、海水、混合水以及埋藏白云岩化作用五种模式。
The research on dolomite genesis is in postulation stage at present, which includes five models of vaporization, infiltration and circumfluence, sea water, mixing water and buried dolomitization.
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