Fig. 13From: Paleomagnetic studies on single crystals separated from the middle Cretaceous Iritono graniteAnisotropy bias calculated from the typical anisotropy tensor of plagioclase samples as a function of angle between two remanence vectors (here assumed to be NRM and ARM0). An anisotropy bias larger than 1 indicates that the paleointensity is overestimated, and vice versaBack to article page