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贵州旦坪铝土矿矿床地质特征及成因探讨

徐彬 张华松 陈建平 王权锋 姚美娟

桂林理工大学学报2017,Vol.37Issue(4):570-579,10.
桂林理工大学学报2017,Vol.37Issue(4):570-579,10.DOI:10.3969/j.issn.1674-9057.2017.04.003

贵州旦坪铝土矿矿床地质特征及成因探讨

Geological features and genesis of bauxite deposit in Danping, Guizhou province

徐彬 1张华松 2陈建平 3王权锋 4姚美娟1

作者信息

  • 1. 成都理工大学数学地质四川省重点实验室,成都610059
  • 2. 贵州省地矿局106地质大队,贵州遵义563000
  • 3. 中国地质大学(北京)地球科学与资源学院,北京100083
  • 4. 中国地质大学(北京)北京市国土资源信息研究开发重点实验室,北京100083
  • 折叠

摘要

Abstract

The bauxite deposit in Danping,located at the Zheng'an bauxite belt,is in the northern part of central Guizhou-southern Chongqing metallogenic belt,an important mineralization with good mineralization conditions.The geological characteristics,ore-controlling factors,mineralization enrichment rules and prospecting criteria of the deposit are analyzed,and the genesis of the deposit is discussed.The results show that it is a sedimentary deposit.Its metallogenic material mainly comes from the mud shale of ore-bearing rock series (Dazhuyuan Formation) sedimentary basement Hanjiadian Group.The bauxite deposit in Danping is a large deposit rich in gallium,estimating resource of 22.289 1 million tons,which is a large bauxite deposit.Among the ore body,the type of low iron high sulfur occupies first place,low iron low sulfur comes second.The main ore is clastic type,then half an earthy,oolitic and massive compacted.All of ore bodies are distributed in the middle-upper part of Dazhuyuan Formation of Middle Permian,which is the most intuitive and important ore-controlling factors in study area.It is also the main criteria and basis of bauxite deposit prospecting and exploitation in this area.

关键词

铝土矿/地质特征/矿床成因/找矿标志/旦坪/贵州

Key words

bauxite deposit/geological features/deposit genesis/prospecting criteria/Danping/Guizhou

分类

天文与地球科学

引用本文复制引用

徐彬,张华松,陈建平,王权锋,姚美娟..贵州旦坪铝土矿矿床地质特征及成因探讨[J].桂林理工大学学报,2017,37(4):570-579,10.

基金项目

数学地质四川省重点实验室开放基金项目(scsxdz201708) (scsxdz201708)

中国地质调查局项目(1212011120997) (1212011120997)

桂林理工大学学报

OA北大核心CSTPCD

1674-9057

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