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贵州威宁窑上组沉积物物源特征及沉积控制因素分析
引用本文:孔凡翠,杨瑞东,韩晓彤,魏怀瑞,程玛丽,高军波,任海利,龙杰.贵州威宁窑上组沉积物物源特征及沉积控制因素分析[J].现代地质,2011,25(3).
作者姓名:孔凡翠  杨瑞东  韩晓彤  魏怀瑞  程玛丽  高军波  任海利  龙杰
作者单位:贵州大学资源与环境工程学院,贵州贵阳,550003
基金项目:国家重点基础研究发展规划"973"项目,贵州大学"211"重点学科建设基金项目
摘    要:根据威宁草海第四纪窑上组沉积物主量元素和REE特征,探讨沉积物物源特征、气候演变情况、沉积物堆积控制因素。结果表明:Al、Mg、Ca、K、Na和Ti的含量变化在剖面上一致,它们的相关系数很高(0.522~0.985)。Fe含量和Mn含量呈正相关形式,与Al、Mg、Ca、K、Na和Ti呈负相关。Fe2O3含量在土黄色粘土的铁质层很高(42.86%~50.57%)。样品中REE球粒陨石标准化配分模式与贵州土壤、贵州碳酸盐岩风化壳配分模式很相似,与峨眉山玄武岩配分模式不一致,但其含量略低于贵州碳酸盐岩风化壳的含量;沉积物主要来源于碳酸盐岩,且碳酸盐岩强烈风化成土作用使REE超常富集,在剖面上呈现高ΣREE(平均219.38μg/g)。通过Mg/Ca、MgO/Al2O3、(CaO+K2O+Na2O)/Al2O3、(Fe2O3+Al2O3)/(MgO+CaO)、(K+Na+Ca+Mg)/(Fe+Mn)、(Al+Fe+Mn)/(K+Ca+Mg)和(MgO+Na2O+CaO)/Al2O3等气候指标研究,表明在草海窑上期为湖泊沉积时期,气候经历了由温暖湿润向冷干的转变。同时,认为物源性质、构造运动、气候等共同控制该区沉积物形成。

关 键 词:物源特征  湖泊沉积物  窑上组  草海  贵州

Analysis of Sediment Provenance and Sedimentary Control Factors in Yaoshang Formation,Weining County in Guizhou Province
KONG Fan-cui,YANG Rui-dong,HAN Xiao-tong,WEI Huai-rui,CHENG Ma-li,GAO Jun-bo,REN Hai-li,LONG Jie.Analysis of Sediment Provenance and Sedimentary Control Factors in Yaoshang Formation,Weining County in Guizhou Province[J].Geoscience——Journal of Graduate School,China University of Geosciences,2011,25(3).
Authors:KONG Fan-cui  YANG Rui-dong  HAN Xiao-tong  WEI Huai-rui  CHENG Ma-li  GAO Jun-bo  REN Hai-li  LONG Jie
Institution:KONG Fan-cui,YANG Rui-dong,HAN Xiao-tong,WEI Huai-rui,CHENG Ma-li,GAO Jun-bo,REN Hai-li,LONG Jie(College of Resources and Environmental Engineering,Guizhou University,Guiyang,Guizhou 550003,China)
Abstract:The feature of major elements and REEs composition of lake sediments of Yaoshang Formation in Guizhou,Weining County,are analyzed.The provenance features,climatic evolution and control factors of sediment accumulation have been discussed.The results show that: The change of abundance of Al,Mg,Ca,K,Na and Ti is consistent in the section.Their correlations between 0.522 and 0.985 are very high.Fe and Mn form a positive correlation,while they negatively correlate with Al,Mg,Ca,K,Na and Ti.The abundance of Fe2O...
Keywords:terrestrial provenance  lake sediment  Yaoshang Formation  Caohai Lake  Guizhou  
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