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黔北铝土矿床K、Na含量比的沉积环境指示意义     被引量:1

Implication of Na/K ratio to the sedimentary environment of bauxite deposits in Northern Guizhou

文献类型:期刊文献

中文题名:黔北铝土矿床K、Na含量比的沉积环境指示意义

英文题名:Implication of Na/K ratio to the sedimentary environment of bauxite deposits in Northern Guizhou

作者:向贤礼 金中国 韩润生 黄智龙 谷静

第一作者:向贤礼

机构:[1]贵州理工学院;[2]贵州省有色金属和核工业地质勘查局;[3]昆明理工大学;[4]中国科学院地球化学研究所

第一机构:贵州理工学院

年份:2014

卷号:28

期号:6

起止页码:685-691

中文期刊名:矿产与地质

外文期刊名:Mineral Resources and Geology

收录:CSTPCD

基金:科技部科技支撑项目"贵州省务正道地区铝土矿勘查技术集成与示范研究"(项目编号:2011BAB04B04)资助

语种:中文

中文关键词:铝土矿;沉积环境;成矿环境;地球化学

外文关键词:bauxite deposit;;sedimentary environments;;metallogenetic environment;;Geochemistry

摘要:岩石矿物的某些地球化学成分可指示特定的成岩成矿环境。在对黔北(道真、务川、正安)铝土矿床的研究中,发现铝土矿石中K2O含量普遍小于Na2O含量。其它沉积环境地球化学标志显示矿床沉积于陆相淡水环境。通过国内铝土矿床的对比研究,认为海相环境形成的铝土矿床K2O/Na2O比值大于1,陆相淡水环境形成的铝土矿床K2O/Na2O比值小于1,反映了K、Na含量比对铝土矿床的沉积环境具有明显的指示意义。
Some of the chemical components of rocks and minerals may indicate certain diagenetic and metallo-genic environment.The study on bauxite deposits in North Guizhou (Daozhen,Wuchuan and Zheng’an) finds that the K2 O content in bauxitic ores is commonly lower than Na2 O content.Other geochemical indica-tors of sedimentary environment show that the deposits precipitate in continental freshwater environment. After comparing the results with other studies of domestic bauxite deposits,the author believes that K2 O/Na2 O ratio of bauxite deposits formed in marine environment is more than 1,whereas K2 O/Na2 O ratio of bauxite deposits formed in continental freshwater environment is less than 1.It is revealed that Na/K ratio is an obvious indicator to the sedimentary environment of bauxite deposits.

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