Fig. 8From: Paleomagnetic studies on single crystals separated from the middle Cretaceous Iritono graniteA representative result of successful paleointensity measurements by the Tsunakawa–Shaw method on single plagioclase grain. The dotted line indicates where the horizontal and vertical axes are equal. In the orthogonal plot, open and closed circles indicate X–Y and X–Z planes, respectivelyBack to article page