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贵州福泉高洞铝土矿床成矿地质地球化学特征

金中国 郑明泓 刘玲 骆军 董光贵 陈兴龙

地质与勘探2018,Vol.54Issue(3):522-534,13.
地质与勘探2018,Vol.54Issue(3):522-534,13.

贵州福泉高洞铝土矿床成矿地质地球化学特征

Geological and Geochemical Characteristics of Mineralization in the Gaodong Bauxite Deposit, Fuquan,Guizhou Province

金中国 1郑明泓 1刘玲 1骆军 2董光贵 1陈兴龙1

作者信息

  • 1. 贵州省有色金属和核工业地质勘查局,贵州贵阳550005
  • 2. 贵州省有色金属和核工业地质勘查局物化探总队,贵州都匀558000
  • 折叠

摘要

Abstract

The bauxite deposit in the Gaodong area of Guizhou Province is one of the newly discovered mid-sized bauxite deposits in recent years.Its ore-bearing strata are the Jiujialu Formation of the Lower Carboniferous.Layered and layered-like bauxite lies on the ancient erosion surface of the car-bonate rocks in the Upper Devonian System,contacting the overlying Liangshan Formation of the Middle Permian System and underlying Gaopochang For-mation of the Upper Devonian System in a disconformable manner.The genesis of the deposit is of an ancient weathering crust depositional type.Analyzing the characteristics of Ga,Ba,Sr and Th contents and B / Ga,Rb / K and V / Zr ratios in the ore-bearing rocks suggests that the bauxite formed in a con-tinental sedimentary setting.The features δCe,Ni / Co,Th / U,Sr / Cu and V / Cr reveal that the diagenesis and mineralization process of the bauxite was in an oxidative environment.The positive correlation between Al and Zr,Hf,Nb,Ta,Th and U in the ore-bearing rocks indicates that the bauxite has the same migration and significant enrichment characteristics.The content of trace elements in the ore-bearing rock series is strongly enriched compared with that of the carbonate rocks of underlying strata Gaopochang Formation.Compared with the value of Li Tong,the high-temperature metallogenic elements (W,Sn,Mo and Bi),high-field strength elements (Nb,Ta,Th,U,Hf and Zr),clay mineral easily adsorbed elements (Li and V) and the high-grade ge-ochemical background element (Sb) in fine-grained rocks are highly enriched.Fractionation of LREE and HREE is obvious.It is inferred that the migra-tion rate of HREE with smaller ionic radius is larger than LREE with larger ionic radius in the process of secondary weathering leaching.

关键词

铝土矿/地质地球化学特征/成矿环境/高洞/贵州/福泉

Key words

bauxite/characteristics of geology and geochemistry/metallogenetic environment/Gaodong area/Guizhou Province/Fuquan

分类

天文与地球科学

引用本文复制引用

金中国,郑明泓,刘玲,骆军,董光贵,陈兴龙..贵州福泉高洞铝土矿床成矿地质地球化学特征[J].地质与勘探,2018,54(3):522-534,13.

基金项目

国家十二五科技支撑计划重点项目(编号:BAB201104B04)、贵州省地勘基金项目(编号:ZZKC2012-06)和贵州省公益性、基础性项目(编号:2016-07)联合资助. (编号:BAB201104B04)

地质与勘探

OA北大核心CSCDCSTPCD

0495-5331

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