Objective Although the occurrence of Late Paleozoic rifting on the northern margin of Gondwana is widely accepted,the precise reason for the rifting is not constrained.The Woniusi basalts in the Baoshan terrane cover ...Objective Although the occurrence of Late Paleozoic rifting on the northern margin of Gondwana is widely accepted,the precise reason for the rifting is not constrained.The Woniusi basalts in the Baoshan terrane cover an area of～1.2×10~4 km~2 and have been considered to be likely part展开更多
基金financially supported by the National Natural Science Foundation of China (grant No. 41703030)research grants from the East China University of Technology (grants No. DHBK2015323, DHBK2012207 and RGET1504)
文摘Objective Although the occurrence of Late Paleozoic rifting on the northern margin of Gondwana is widely accepted,the precise reason for the rifting is not constrained.The Woniusi basalts in the Baoshan terrane cover an area of～1.2×10~4 km~2 and have been considered to be likely part
