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华北克拉通在形成和演化中经历的最重要的地质事件发生在 ２ ６００～２ ４００和２ ０００－１７００ Ｍａ期间（简称 ２５亿年地质事件和 １８亿年地质事件）．提出这两个事件的实质是：古老的微陆块以规模较小的板块构造形式拼合成超大陆，以及超大陆受古地幔柱构造的影响再裂解成不同的陆块．
The most important geological events experienced during the formation and evolution of the North China Craton occurred between 2,600 and 2,400 and 2,000 and 1,700 Ma (2.5 billion geological events and 1.8 billion geological events for short). The essence of these two incidents is that the ancient micro-continental blocks have been spelled into the supercontinent in the form of smaller plate tectonics, and the supercontinent has been cracked into different land masses under the influence of the ancient mantle plume structure.