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Fig. 5 | Earth, Planets and Space

Fig. 5

From: Paleomagnetic studies on single crystals separated from the middle Cretaceous Iritono granite

Fig. 5

Results 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/T

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