Based on the high-resolution studies on Holocene loess-palaeosol sequence, we studied the Holocene pedogenic environment evolution in Fen-wei plains of loess plateau from the angle of quaternary geology and pedology.
本文在了解国际国内的地学界和环境学界全新世环境演变研究进展的基础上，选定汾渭平原全新世成壤环境演变高分辨率研究作为课题，从第四纪地质和土壤学角度开展研究。
参考来源 - 汾渭平原全新世成壤环境演变的高分辨率研究·2,447,543篇论文数据，部分数据来源于NoteExpress
通过本文各指标的研究，进一步认识了汾渭平原全新世土壤的类型、成因与质量演变。
The soil type, cause of soil formation and soil quality changes of Holocene loess-soil sequence have been clearly distinguished.
地面沉降的重灾区主要是长江三角洲地区、华北平原和汾渭盆地。
The Yangtze River Delta, North China Plain and Fenhe-Weihe Basin are the most severely affected regions.
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