Journal of Geographical Sciences

Figure/Table detail

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

Journal of Geographical Sciences, 2026, 36(1): 177-198. DOI: 10.1007/s11442-026-2443-7

Section	Layer/Period	Regression equations
HZ	Paleosol	χ_pedo=12.5×χ_fd
	Paleosol	χ₀=χ_lf-12.5×χ_fd
	Other layers	χ_pedo=8.61×χ_fd
	Other layers	χ₀=χ_lf-8.61×χ_fd
	6.0-3.5 ka	χ_pedo=6.28×χ_fd
	6.0-3.5 ka	χ₀=χ_lf-6.28×χ_fd
MR	Paleosol I	χ_pedo=21.37×χ_fd
	Paleosol I	χ₀=χ_lf-21.37×χ_fd
	Paleosol II	χ_pedo=13.27×χ_fd
	Paleosol II	χ₀=χ_lf-13.27×χ_fd
	Other layers	χ_pedo=1.86×χ_fd
	Other layers	χ₀=χ_lf-1.86×χ_fd
	6.0-3.5 ka	χ_pedo=19.49×χ_fd
	6.0-3.5 ka	χ₀=χ_lf-19.49×χ_fd

Table S1 Linear regression equations for calculating lithogenic (χ₀) and pedogenic (χ_pedo) magnetic susceptibility components

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