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地壳运动和岩浆活动,是地球内部和外部矛盾各方面相互斗争的反映。构成大陆地壳主体之一的中国广大陆壳,在其漫长的地质发展过程中,经历了十分剧烈、复杂而有规律的构造运动、岩浆活动和成矿作用。与其它地区相比,中国陆壳具有自己的构造特征、岩浆类型与成矿特点,但它的发生、发展又不是孤立的,而是与整个地壳,特别是相邻地区陆壳的演化历史有着紧密的相互联系。
Crustal movement and magmatic activity are a reflection of the mutual struggle between the contradictions inside and outside the Earth. The vast continental crust in China, which constitutes one of the main continental crusts, underwent intense, complicated and regular tectonic movements, magmatic activities and mineralization during its long geological development. Compared with other regions, the continental crust in China has its own structural features, magmatic types and mineralization characteristics. However, its occurrence and development are not isolated. Instead, it is related to the evolution history of the entire crust, especially the adjacent continental crust Closely linked.