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.
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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