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豫西偃师-龙门地区铝土矿三水铝石的赋存特征及成因分析

曹高社 毕景豪 邢舟 杜欣 周红春 陈永才

河南理工大学学报(自然科学版)2018,Vol.37Issue(2):44-52,9.
河南理工大学学报(自然科学版)2018,Vol.37Issue(2):44-52,9.DOI:10.16186/j.cnki.1673-9787.2018.02.007

豫西偃师-龙门地区铝土矿三水铝石的赋存特征及成因分析

Occurrence characteristics and genesis of the gibbsite in bauxite in Yanshi-Longmen area, western Henan province

曹高社 1毕景豪 2邢舟 1杜欣 1周红春 3陈永才3

作者信息

  • 1. 河南理工大学 资源环境学院,河南焦作454000
  • 2. 中原经济区煤层(页岩)气河南省协同创新中心,河南焦作454000
  • 3. 河南省地矿局第四地质勘查院,河南郑州450001
  • 折叠

摘要

Abstract

Gibbsite is newly discovered in the surface outcrop of the Benxi Formation in Yanlong area,western Henan province.The discovery provides direct evidence for the existence of karst accumulated bauxite,and also has significance theoretical values for analyzing its characteristics and genesis.The newly discovered gibbsite mainly occurred in the white and red sedimentary bands that is convergence zone of Majiagou Formation limestone,Benxi Formation and variegated bauxitic mudstone of Benxi Formation.X-Ray diffraction analysis,differential thermal analysis and SEM-EDS analysis were conducted to those above-mentioned sedimentary bands and bauxitic mudstone.The results show that the gibbsite has typical X-Ray diffraction characteristic peaks and differential thermal absorption peaks of gibbsite,which appers banded structure at macro level and compact aggregates at microscopic level.Based on the principles of soil geochemistry,we conclude that the gibbsite is the mineral of the ferrallitization after Benxi Formation bauxite was uplifted to the surface.

关键词

铝土矿/三水铝石/成因/本溪组/豫西

Key words

bauxite/gibbsite/genesis/Benxi Formation/western Henan province

分类

矿业与冶金

引用本文复制引用

曹高社,毕景豪,邢舟,杜欣,周红春,陈永才..豫西偃师-龙门地区铝土矿三水铝石的赋存特征及成因分析[J].河南理工大学学报(自然科学版),2018,37(2):44-52,9.

基金项目

国土资源部全国油气资源战略选区调查与评价项目(1211302108023-2) (1211302108023-2)

河南省两权价款项目(20111-36-8) (20111-36-8)

河南理工大学学报(自然科学版)

OA北大核心CSTPCD

1673-9787

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