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Spatiotemporal heterogeneity of magnetic enhancement mechanisms in aeolian deposits on the southern Tibetan Plateau: Implications for paleoclimatic reconstruction in mountain- basin systems
WANG Haoyu, YANG Junhuai, QU Wenxi, WANG Linkai, ZHANG Canyi, LIU Xin, TANG Jinmeng, GAO Fuyuan, CHEN Zixuan, WANG Shuyuan, FAN Yijiao, WU Duo
地理学报(英文版), 2026, 36(1): 177-198.   DOI: 10.1007/s11442-026-2443-7

Section Layer/Period Regression equations
HZ Paleosol χpedo=12.5×χfd
χ0lf-12.5×χfd
Other layers χpedo=8.61×χfd
χ0lf-8.61×χfd
6.0-3.5 ka χpedo=6.28×χfd
χ0lf-6.28×χfd
MR Paleosol I χpedo=21.37×χfd
χ0lf-21.37×χfd
Paleosol II χpedo=13.27×χfd
χ0lf-13.27×χfd
Other layers χpedo=1.86×χfd
χ0lf-1.86×χfd
6.0-3.5 ka χpedo=19.49×χfd
χ0lf-19.49×χfd
Table S1 Linear regression equations for calculating lithogenic (χ0) and pedogenic (χpedo) magnetic susceptibility components
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