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

Figure S7 Correlations between magnetic parameters and sedimentological proxies. (a-c) Magnetic susceptibility (χlf) versus the >63 μm fraction for all samples in the SGX, HZ, and MR sections, respectively. (d) χlf versus the >63 μm fraction for samples dated to 6.0-3.5 ka in the SGX section. (e-f) χlf versus frequency-dependent magnetic susceptibility (χfd) for samples dated to 6.0-3.5 ka in the HZ and MR sections, respectively. Pearson correlation coefficients (R) and their statistical significance (**p < 0.01) are indicated.
Other figure/table from this article