Caledonian orogeny

基本解釋

After the Caledonian orogeny, South China 'was uplifted except for the Qinzhou-Fangchen area of Guangxi existing as a remain trough.
加里東運(yùn)動(dòng)結(jié)束后，華南廣大地區(qū)上升成陸，僅欽防一線為殘留海槽。
After the Caledonian orogeny, the Yangtze plate and the Cathaysia landmass were matched together to be the united plate of south China.
加里東運(yùn)動(dòng)以后，揚(yáng)子和華夏陸塊拼合成統(tǒng)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里東運(yùn)動(dòng)期間遭受了變形變質(zhì)作用，形成了一套片巖—片麻巖—混合巖系變質(zhì)巖。