对亚热带峨眉山、天目山和凤阳山的系列样品研究表明,高、低海拔土壤在矿质风化与淋溶、氧化铁富集与转化、粘粒矿物类型及分布等方面均酷为相似,而这些地球化学特性在相同温差水平带的土壤上却有明显区别,由此推算的新构造运动强度与前人研究结果基本一致。这对阐明山地土壤的发生分类及拓宽新构造运动研究方法等有一定参考价值。

The results of the study show that the characteristics of soil situated at low altitude in weathering and leaching, enrichment of Fe₂O₃ and its morphological transformation and clay mineral types are extremely similar to the soil located at high altitude in Emei Mountain, Tianmu Mountain and Fengyang Mountain.