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银川盆地晚第四纪环境特征
引用本文:童国榜 宋祥华. 银川盆地晚第四纪环境特征[J]. 地球科学, 1995, 20(4): 421-426
作者姓名:童国榜 宋祥华
作者单位:地质矿产部水文地质工程地质研究所,宁夏回族自治区地质矿产局第一水文地质工程地质大队,中国科学院武汉岩土力学研究所
摘    要:依据银川盆地8个钻孔的第四系的研究,对该区近12万年的自然环境特点进行了探讨。结果表明:该时期植要是在森林草原与草原类型间频荒漠草原4个发展阶段,其中短时间尺度的植被演替主要是在森林草原与草原类型间频繁发生。

关 键 词:晚第四纪 古环境 古气候 银川盆地

ENVIRONMENT FEATURES OF YINCHUAN BASIN IN LATE QUATERNARY PERIOD
Tong Guobang,Shi Ying, Fan Shuxian,Zhang Junpai. ENVIRONMENT FEATURES OF YINCHUAN BASIN IN LATE QUATERNARY PERIOD[J]. Earth Science-Journal of China University of Geosciences, 1995, 20(4): 421-426
Authors:Tong Guobang  Shi Ying   Fan Shuxian  Zhang Junpai
Abstract:Based on the achievements in the Quaternary research of eight 300m-depth drill holes in Yinchuan Basin(including paleogeomagnetism, 14C dating,spore-pollen analysis and the structure analysis in surface of quartz grains),the changes of natural environment of Yinchuan Basin in 120ka are studied in this paper.It indicates that paleo-vegetation have gone through forest-sylvosteppe-steppe-desert steppe stages,in these stages, the short-time vegetation succession happened frequently between sylvosteppe and steppe.Correspondingly,paleoclimate had gone through warm/wet -cool/wet -cold/dry warm/dry process,and the match of cold/warm and dry/wet climates was very complicated in the second flucturate of climate.The evolutions of vegetation and climate showed that dry environment happening was of stage character. In geology history,the short-term drought began from 30kaB.P.,and the climate was cold/dry before this period,and was warm/dry after this period.
Keywords:Late Quaternary  paleoenvironment  paleoclimate  Yinchuan Basin.  
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