原生岩浆是高镁拉斑玄武岩浆。
浙江新生代玄武岩主要岩石类型为橄榄拉斑玄武岩。
The chief type of Cenozoic basalts in Zhejiang is of olivine-tholeiites.
绿片岩原岩是一套含板内拉斑玄武岩的火山沉积建造。
The greenschists originated from a series of volcanic - sedimentary formations with intercalated intracontinental tholeiites.
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