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应用构造—岩性—事件法将五台山碰撞造山带划分为３个构造片体：弧前混杂岩带、古岛弧系和弧后混杂岩带。提出该造山带构造演化５个阶段：洋盆扩张阶段（＞２６００Ｍａ）；南部洋盆向微陆块下俯冲—微陆块转化为岛弧阶段（２６００～２５００Ｍａ）；弧前碰撞—弧后消减阶段（２５５０～２５００Ｍａ）；陆—陆碰撞阶段（２５５０～２４５０Ｍａ）；伸展作用阶段（２５００～２４００Ｍａ）。
Using the tectono-lithology-event method, the Wutaishan collision orogenic belt is divided into three tectonic slices: pre-arc melange belt, ancient island arc system and backarc melange belt. The tectonic evolution of the orogenic belt is proposed to be characterized by five stages of tectonic evolution: ocean basin expansion (> 2600Ma); subduction of micro-continental blocks in the southern ocean basin-micro-continental blocks to island arc (2600-2500Ma) Stage (2550 ~ 2500Ma); continental-continental collision stage (2550 ~ 2450Ma); stretching stage (2500 ~ 2400Ma).