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安徽淮北平原晚更新世以来地质环境与土壤发育
引用本文:王长荣,顾也萍.安徽淮北平原晚更新世以来地质环境与土壤发育[J].安徽师范大学学报(自然科学版),1995,18(2):59-65.
作者姓名:王长荣  顾也萍
摘    要:本文主要讨论安徽淮北平原更新世以来地质环境的演变,及其相关沉积物的特征,并从成土母质,地貌特征和水文地质等成土因素的差异,探讨淮北平原土壤的发育和分布规律。

关 键 词:地质环境  土壤发育  晚更新世

Geologic Environment after Late Pleistoscene and Soil Development in Huaibei Plain of Anhui
Wang Changrong, Gu Yeping.Geologic Environment after Late Pleistoscene and Soil Development in Huaibei Plain of Anhui[J].Journal of Anhui Normal University(Natural Science Edition),1995,18(2):59-65.
Authors:Wang Changrong  Gu Yeping
Institution:Department of Geography
Abstract:This paper discuss the evolution of geologic environment after late pleis-toscene and the features of concerned deposit material mainly.According to the differ-ence of soil-formation factors in soil parent material and geomorphic features and hy-drogeology etc,the treatise approach soil development and the law of soil distribution inHuaibei plain of Anhui proivnce
Keywords:Geologic environment  soil development  late pleistoscene  Huaibei plain    
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