摘要
By abundant polished thin section lithofacies and mineralgraphy study to the drills, tunnels and limited surface outcrop rock simple in southwest Guizhou and northwest Guangxi, and the study of 6 element pairs of petrochemistry, microelement, REE, W(Th)/W(U) and so on, it’s proved that the main material of Longtan Formation above the Dachang layer is from the basaltic volcanic clastic material. The ratio of the element pairs shows that the source mainly is the mantle, the trace element comparison is the same to the Emeishan basalt. Its litholgy should be basaltic tuffite, has closely related with Emeishan basalt erupted in the same era.