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.
在广东东部是一套陆相沉积—火山岩复理石建造。
There is a continental sedimentary-volcanic flysch formation in eastern Guangdong.
其上部为一套变质的复理石建造，下部为变质的火山-沉积岩建造。
The upper part of it is a suit of metamorphic flysch formation, and the lower part, metamorphic volcanic-sedimentary rocks.
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