Fig. 11From: Paleomagnetic studies on single crystals separated from the middle Cretaceous Iritono graniteSummary of paleointensity and error (1σ) of plagioclase compared with the whole rock. Black circles indicate results of each plagioclase grain. Green circle denotes the mean of nine plagioclase grains. Red square marks the mean of whole-rock measurements (Tsunakawa et al. 2009)Back to article page