论文信息 - The 2.31 Ga mafic dykes in the Karelian Craton, eastern Fennoscandian shield: U–Pb age, source characteristics and implications for continental break-up processes - 字舞流文

The 2.31 Ga mafic dykes in the Karelian Craton, eastern Fennoscandian shield: U–Pb age, source characteristics and implications for continental break-up processes

A. V. Stepanova | E. B. Sal’nikova | S. Egorova | V. Stepanov | A. Samsonov | Y. Larionova | A. Stepanova | E. Sal’nikova