华南新元古代到早古生代是扬子活动大陆边缘构造“捕获”的一个边缘海盆地，其间充填了巨厚的复理石、砂、页岩沉积。
During the Neoproterozoic to the Early Paleozoic, the South China was a marginal basin captured by the Yangtze active continental margin, filled with very thick flysch, sandstone, and shale sediments.
新元古代和古生代盆地具有一系列相同的地质特征。
The Neoproterozoic to Paleozoic basins share a number of common geological features.
古生代的 意思是“古代生命”，中生代的意思是“中间的生命”，而新生代意即“新的生命”。
The Palaeozoic which means "ancient life", the Mesozoic which means "middle life"and the Cenozoic which means "recent life".
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