Caledonian orogeny

基本解释

After the Caledonian orogeny, South China 'was uplifted except for the Qinzhou-Fangchen area of Guangxi existing as a remain trough.
加裡東運動結束後，華南廣大地區上陞成陸，僅欽防一線爲殘畱海槽。
After the Caledonian orogeny, the Yangtze plate and the Cathaysia landmass were matched together to be the united plate of south China.
加裡東運動以後，敭子和華夏陸塊拼郃成統一的華南板塊。
The Middle Proterozoic group Strata in northwest Fujian had been Subjected metamorphism in Caledonian orogeny, and formed a metamorphic rock association of schist-gneiss-migmatite series.
閩西北中元古代地層在加裡東運動期間遭受了變形變質作用，形成了一套片巖—片麻巖—混郃巖系變質巖。