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赣南地处华南褶皱系之万洋山——诸广山拗褶断带与武夷山隆褶断带。古生代阶段属古亚洲构造域,中生代阶段属滨太平洋构造域。崇余饶地区则位于万洋山——诸广山拗褶断带内次级北北东向复式向斜的东翼。区域经历了多阶段的强烈构造运动,而几乎每次重要的地壳构造运动,都有相应的岩浆岩形成,具有多旋回岩浆活动特征。
Gannan is located in the Wanyangshan-Zhuangshan fault fold belt and the Wuyishan long fold belt in the South China fold system. Paleozoic stage is an ancient Asian tectonic domain, the Mesozoic stage is the Pacific tectonic domain. The Chongyu Rao area is located in the east wing of the subordinate north-easterly trending syncline within the Wanyangshan-Zhuangshan fault fold belt. The region experienced multi-stage intense tectonic movement, and almost every important crustal movement has corresponding magmatic rock formation with multi-cycle magmatic activity.