Detailed micromorphological analysis indicates that the micro-texture in the Holoence loess-palaeosol sequence in the southern Loess Plateau is divided into cementing texture and granular texture.

• 通过对土壤微结构系统的研究,发现黄土高原南部全新世黄土-古土壤序列的微结构可分为基底式胶结结构、胶斑状结构、斑状-胶斑结构、粒状结构、似粒状结构和粒状-斑状结构。