Fig. 9
From: A paleomagnetic record in loess–paleosol sequences since late Pleistocene in the arid Central Asia
Comparison of inclination record in the BYH section (c) with Xining (a) (XN, Zhu et al.1994) and Jiuzhoutai (b) (JZT, Fang et al. 1997) sections. The RPI record comparison between the Xining section (d) and the BYH section (e) (Zhu et al. 1994). f Virtual geomagnetic poles (VGPs) for the depth interval (9.1–9.9 m and 29.2–30.4 m) that contains the BGE (red) and LGE (blue), respectively, in the BYH section