Fig. 5From: Paleomagnetic studies on single crystals separated from the middle Cretaceous Iritono graniteResults of experiments on selected quartz. a, b Stepwise ThD of NRM. In the orthogonal plot, open and closed circles indicate X–Y and X–Z planes, respectively. c Low-temperature remanence measurements. Solid lines for ZFC measurements and dotted lines for FC measurements. d Hysteresis loop after slope correction. The slope correction coefficient was + 74.8 nAm2/TBack to article page