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广西运动作为华南地质重要概念之一，已建立７０年，一般被认作志留纪末华夏地块和扬子地块会聚而致的造山运动．据广西及邻区地质研究新进展，桂西和桂中柳州－合山地区早古生代属于稳定地块．广西运动起因于寒武纪末南面云开地块向北挤压，形成其间的大明山－大瑶山褶皱带，可能与晚泛非运动相关。华夏地块和扬子地块会聚过程发生在晚奥陶世～早志留世，影响范围主要在湘、赣两省，可用崇余运动称之．志留纪末无造山运动．
As one of the important concepts of geology in South China, the Guangxi movement has been established for 70 years and is generally regarded as a orogenic movement resulting from the convergence of the Silurian massif and the Yangtze block. According to recent advances in geological research in Guangxi and its adjacent areas, the Early Paleozoic in the Liuzhou-Heshan area of Guangxi and Guangxi provinces belonged to a stable block. The Guangxi movement was caused by the northward extrusion of the southern Yunnan block in the Cambrian Period, forming the Damingshan-Dayao Mountain fold belt in the meantime, possibly related to late pan-non-movement. The convergence process of the Huaxia block and the Yangtze block occurred in the Late Ordovician ~ Early Silurian, with the scope of influence mainly in Hunan and Jiangxi Provinces, which can be called the Chongyu Campaign. Silurian no orogeny at the end.