通过对前寒武纪建造、构造的综合分析研究认为：中元古代晚期浙西-赣东北地区是华夏古陆的活动陆缘；武陵运动是华南一次最重要的造山运动，华夏古陆与扬子地块沿赣东北断裂带发生碰撞，形成了统一的“华南古大陆”。 Based on a comprehensive analysis of the Precambrian construction and tectonics, it is concluded that the late Western Central Plains was from the western Zhejiang to the northeast of Jiangxi in the active continental margin of the Cathaysia; the Wuling movement was the most important orogeny in southern China, The block collided along the northeastern Jiangxi fault zone, forming a unified “southern China ancient continent.”