Fig. 5From: A paleomagnetic record in loess–paleosol sequences since late Pleistocene in the arid Central AsiaOrthogonal vector projections obtained from THD of typical samples (modified from Li 2016). a Typical sample at the depth of 5.6 m, b typical sample at the depth of 9.4 m, c typical sample at the depth of 13.8 m, d typical sample at the depth of 16.3 m, e typical sample at the depth of 24.9 m, and f typical sample at the depth of 29.5 m in the BYH section. Red lines indicate the stable component isolated by thermal demagnetizationBack to article page