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湖南古丈县万岩重晶石矿床地质特征及找矿前景

刘丙秋

化工矿产地质2016,Vol.38Issue(2):115-119,5.
化工矿产地质2016,Vol.38Issue(2):115-119,5.

湖南古丈县万岩重晶石矿床地质特征及找矿前景

GEOLOGICAL FEATURES OF WANYAN BARITE ORE IN GUZHANG HUNAN MINERAL OCCURRENCE AND ORE-FINDING

刘丙秋1

作者信息

  • 1. 中化地质矿山总局湖南地质勘查院,湖南长沙 410000
  • 折叠

摘要

Abstract

Wanyan Barite Ore point in Guzhang is newly discovered mineralization point when carry out Hunan Guzhang region mineral prospective survey. The genesis of the deposit can be speculated as low temperature hydrothermal deposit. The Ore genesis are complete controlled by fissure. The ore-bearing stratum is early Sinian System Jinjiadong Group(Z2j),the phosphorite in middle part of this stratum and the pyrite in the bottom of the same stratum is easily identified in field observation and the consanguineous spatial relationship with Barite Ore body has important indicator for prospecting. Its east there may be a certain size of ore body with some prospecting prospect.

关键词

万岩/重晶石/矿床成因/找矿标志

Key words

Wanyan/Barite/Ore genesis/prospecting marks

分类

天文与地球科学

引用本文复制引用

刘丙秋..湖南古丈县万岩重晶石矿床地质特征及找矿前景[J].化工矿产地质,2016,38(2):115-119,5.

基金项目

本文为中国地质调查局地质调查项目“湖南古丈地区矿产地质调查(项目编号12120113062700)”部分成果。 ()

化工矿产地质

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