沙漠、戈壁和黄土表土岩石磁学特征及其对黄土磁化率机制的意义
毛学刚, 赵丽娟

Rock magnetic properties of deserts, gobi and loess topsoils and their implications in models of magnetic susceptibility
Xuegang Mao, Lijuan Zhao
图2 戈壁和黄土表土粒度频率分布(沙漠粒度总体>1 000 μm,没有经过激光粒度仪测量)
Fig.2 The particle size distributions of Gobi and loess topsoil. The particle size of deserts is greater than 1 000 μm, not measured using Masters2000