Fig. 8From: A paleomagnetic record in loess–paleosol sequences since late Pleistocene in the arid Central Asia(Reproduced with permission from Li et al. 2016)Magnetostratigraphy results of the BYH loess section. The polarity zonation is defined by inclination and declination of the ChNRM derived from continuous four points with PCA. Tie point ages are shown at the left side, obtained by radiocarbon dating (AMS), and optically stimulated luminescence dating of quartz (OSL) and feldspar (pIRIR).Back to article page