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.
礼岷前陆盆地经历了早期深海—半深海的复理石沉积阶段和晚期陆相磨拉石沉积阶段。
The Lixian-Minxian foreland basin undertook abyssal-bathyal flysch deposition at its earlier evolution stage and continental molasse stage at its later evolution stage.
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