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华北克拉通古元古代区域构造至少可以划分出三大构造单元：（１）陆内裂谷带（２．３０～２．６０Ｇａ）；（２）陆缘造山带（２．３０～２．６０Ｇａ）；（３）再造的太古代克拉通区（麻粒岩相带）（大于２．５０Ｇａ）．太古代末—古元古代重要的区域性构造－热事件序列依次为：（１）克拉通中部不同地壳层次伸展及裂谷盆地的发育；（２）克拉通北缘构造活动、增生及陆壳基底再造；（３）与大陆裂谷盆地闭合过程相联系的板内造山－前陆盆地发育．板块构造模式可以很好地解释上述构造作用类型．
The Paleoproterozoic regional structure of North China Craton can be divided into at least three tectonic units: (1) intracontinental rift zone (2.30 ~ 2.60Ga); (2) continental margin orogeny (2.30 ~ 2.60Ga ); (3) Reconstructed Archean cratonic zone (granulite facies belt) (greater than 2.50 Ga). Late Archean-Important Palaeozoic regional tectono-thermal event sequences were as follows: (1) the extension of different crustal gradations and rift basins in the central craton; (2) the tectonic activities in the northern margin of the craton, Rebuilding; (3) intraplate orogeny-foreland basin associated with the closing process of the rift basins in the continent. Plate tectonic mode can well explain the type of tectonic action mentioned above.