The chief type of Cenozoic basalts in Zhejiang is of olivine-tholeiites.
浙江新生代玄武岩主要岩石类型为橄榄拉斑玄武岩。
2
The greenschists originated from a series of volcanic - sedimentary formations with intercalated intracontinental tholeiites.
绿片岩原岩是一套含板内拉斑玄武岩的火山沉积建造。
3
Compared with the dominant tholeiites the alkaline volcanics from Dongchuan district are less enriched in LREE, probably resulting from earlier melting events in their source.