巴丹吉林沙漠地层序列的粒度分布及其组分成因分析

郭峰, 孙东怀, 王飞, 李再军, 李宝锋. 巴丹吉林沙漠地层序列的粒度分布及其组分成因分析[J]. 海洋地质与第四纪地质, 2014, 34(1): 165-173. doi: 10.3724/SP.J.1140.2014.01165
引用本文: 郭峰, 孙东怀, 王飞, 李再军, 李宝锋. 巴丹吉林沙漠地层序列的粒度分布及其组分成因分析[J]. 海洋地质与第四纪地质, 2014, 34(1): 165-173. doi: 10.3724/SP.J.1140.2014.01165
GUO Feng, SUN Donghuai, WANG Fei, LI Zaijun, LI Baofeng. GRAIN-SIZE DISTRIBUTION PATTERN OF THE DEPOSITIONAL SEQUENCE IN CENTRAL BADAIN JARAN DESERT AND ITS GENETIC INTERPRETATION[J]. Marine Geology & Quaternary Geology, 2014, 34(1): 165-173. doi: 10.3724/SP.J.1140.2014.01165
Citation: GUO Feng, SUN Donghuai, WANG Fei, LI Zaijun, LI Baofeng. GRAIN-SIZE DISTRIBUTION PATTERN OF THE DEPOSITIONAL SEQUENCE IN CENTRAL BADAIN JARAN DESERT AND ITS GENETIC INTERPRETATION[J]. Marine Geology & Quaternary Geology, 2014, 34(1): 165-173. doi: 10.3724/SP.J.1140.2014.01165

巴丹吉林沙漠地层序列的粒度分布及其组分成因分析

  • 基金项目:

    国家重点基础研究发展规划(2010CB833401);国家创新群体计划项目(4012106);国家杰出青年基金项目(40625009)

详细信息
    作者简介: 郭峰(1987-),男,硕士研究生,研究方向为新生代沉积与环境变化,E-mail:guof_10@lzu.cn
    通讯作者: 孙东怀, dhsun@lzu.edu.cn
  • 中图分类号: P531

GRAIN-SIZE DISTRIBUTION PATTERN OF THE DEPOSITIONAL SEQUENCE IN CENTRAL BADAIN JARAN DESERT AND ITS GENETIC INTERPRETATION

More Information
  • 对巴丹吉林沙漠腹地WEDP02孔310.45 m的岩心进行了高分辨率的激光粒度测量,运用Normal和Weibull函数对全孔的粒度分布进行了拟合和组分分离,在结合野外沉积相判断的基础上,将组分的粒径-频率、含量-频率变化作为组分成因分析的依据,系统分析了WEDP02孔沉积序列的粒度组分的成因。结果表明:WEDP02孔沉积物主要以风成砂、湖泊-风成砂混合沉积、冲洪积-风成砂混合沉积为主。风成沉积物中,超细粒成壤、高空远源粉尘、低空近源粉尘、风成砂与风成粗砂组分的粒径界线为2、12、105和270 μm,粉尘与风成砂组分的比例平均值为20%/80%,在粒度组分的粒径-含量投影图中占据右上角部分;湖相沉积物中超细粒化学、悬移及风成砂组分的粒径界线为4、45、150~230 μm,湖相悬移组分含量大于35%,同时可含有风成组分和湖相砂,在粒度组分的粒径-含量投影图中占据细粒下部分;冲洪积超细粒化学、悬移黏土、悬移粉砂、风成砂、冲洪积砂的粒径界线为2、12、80、150~200和300 μm。这些特征反映了巴丹吉林沙漠不同沉积物的沉积学特征,是沉积物成因分析的粒度依据。
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出版历程
收稿日期:  2013-06-18
修回日期:  2013-07-12

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