Fig. 8From: Paleomagnetic directional groups and paleointensity from the flood basalt in the Tarim large igneous province: implications for eruption frequencyRepresentative paleointensity experiment shown on the Arai diagrams. Triangles represent the pTRM checks. Lines indicate least-squares fits to estimate paleointensity. The insets show the Z-step data on the orthogonal vector plots. Green dashed line indicates the principal component fit of the direction. Samples are unoriented relative to the geographic coordinate. a A successful result of whole-rock sample. b A failed result of whole-rock sample. c, d Successful results of single plagioclase samples. e, f Failed results of single plagioclase samplesBack to article page