Mafic dykes have been long considered possible tectonostratigraphic markers in East Antarctica because they are largely confined to Archaean–Early Proterozoic cratonic blocks but are absent from mid-to late Proterozo...Mafic dykes have been long considered possible tectonostratigraphic markers in East Antarctica because they are largely confined to Archaean–Early Proterozoic cratonic blocks but are absent from mid-to late Proterozoic or展开更多
基金supported by Russian Foundation for Basic Research grant 15-05-02761 to EVM
文摘Mafic dykes have been long considered possible tectonostratigraphic markers in East Antarctica because they are largely confined to Archaean–Early Proterozoic cratonic blocks but are absent from mid-to late Proterozoic or
