Fig. 8From: New absolute paleomagnetic intensity data from Cenozoic basalts of Northeast China and exploring rock-magnetic parameters for efficient sample preselection on the Tsunakawa–Shaw paleointensity methodComparisons of distributions in the respective Ms-T parameters, ITC50 (a) and ITC|m| (b), between the TS API “success” and “failure” data subsets. See Fig. 7 for detailed descriptions of these diagramsBack to article page