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| 中国东南地洼区的变质作用类型及其与壳体演化的关系 | |
| 引用本文： | 潘传楚.中国东南地洼区的变质作用类型及其与壳体演化的关系[J].大地构造与成矿学,1994,18(4):321-330. |
| 作者姓名： | 潘传楚 |
| 摘 要： | 本文论述了东南地洼区的五种变质作用类型：接触变质作用、动力变质作用、区域变质作用、混合岩化作用和成矿变质作用；探讨了它们与华南亚壳体的演化－运动史的关系；总结了华南亚壳体自身演化－运动及其与相邻壳体相互影响而产生的变质作用的特征。 |
| 关 键 词： | 东南地洼区，壳体演化，接触变质，动力变质，成矿变质，区域变质，混合岩化，变质作用特征 |
TYPES OF METAMORPHISM IN THE SOUTHE-EAST CHINA DIWA REGION AND THEIR RELATIONSHIP WITH CRUSTOBODY EVOLUTION-MOVEMENTS |
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| Abstract: | This paper discourses on five the types of metamorphism in the of Eastsouthern China diwa region,that is,contact metamophism,dynamic metamorphisn,regional metemorphism,migmatization and mineral-forming metamoephism,and researches their relation with the evolution-movements of Southeast China of the suberustobody,suberustobody and The effect of its neighboring crustobodies. |
| Keywords: | Southeast China diwa region Crustobody evolution Contact metamorphism regional metomorphism dynamic metamorphism migmatization mineral-forming metamorphism metamorphic features |
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