图/表 详细信息

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

Figure 6 Composite lithostratigraphic and multiproxy records for the SGX, HZ, and MR sections, plotted on a common age scale. The cyan bar corresponds to the 6.0-3.5 ka interval. (a) Variations in magnetic parameters and the >63 μm fraction of the SGX section. (b) Variations in magnetic parameters, element ratios, and the >63 µm fraction of the HZ section. (c) Records of magnetic parameters and >63 µm fraction of the MR section, along with the stalagmite δ18O record from Dongge Cave as a proxy for reflecting ISM intensity (Wang et al., 2005).
本文的其它图/表