麻粒岩(granulite)又称粒变岩,是一种变质岩,属中高级区域变质作用产物,是以含紫苏辉石为特征的区域变质岩石。主要分布在太古宙至早元古代变质岩系中。冀东、辽西比较发育。
The rheological study of granulite from continental lower crust is one of the scientific problems,which reveals the crustal deformation,crust-mantle exchange,and deep lithosphere dynamic process.
大陆下地壳麻粒岩的流变学研究可以解释地壳变形、壳幔物质交换以及岩石圈深部动力学过程等科学问题。
参考来源 - 大陆下地壳麻粒岩的流变学研究进展·2,447,543篇论文数据,部分数据来源于NoteExpress
表明麻粒岩可以形成在低密度CO_2之中。
It shows that the granulites are formed under lower density CO2 condition.
攀西麻粒岩是扬子陆块西缘康定杂岩的重要代表。
The Panxi granulite is the most important part of Kangding complex.
河北省宣化地区的高压麻粒岩带是非常具有研究意义的。
The high pressured granulite belts in the Xuanhua area of Hebei Province are very worthy of being studied.
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