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河南黄金山重晶石矿床地质特征与矿床成因

郭钢阳 崔东豪

中国非金属矿工业导刊Issue(1):66-70,5.
中国非金属矿工业导刊Issue(1):66-70,5.

河南黄金山重晶石矿床地质特征与矿床成因

Geological Characteristics and Genesis of the Huangjinshan Barite Deposit in Henan Province

郭钢阳 1崔东豪2

作者信息

  • 1. 河南省第三地质勘查院有限公司,河南 郑州 450014||中共河南省委党校,河南 郑州 453002
  • 2. 河南省第一地质矿产调查院有限公司,河南 洛阳 471026
  • 折叠

摘要

Abstract

The Huangjinshan barite mine is located on the southern edge of the North China platform,with superior geological conditions for mineralization.The barite deposit occurs in the andesite of the Majiahe formation of the Xiong'er group,and two industrial ore bodies are circled.The types of wall rock alteration near the mine include silicification,sericitization,chloritization,carbonation,etc.Among them,silicification,carbonation,and chloritization are closely related to mineralization.The prospecting indicators include fault structure indicators and rock alteration indicators.The Huangjinshan barite deposit is controlled by factors such as fault structure,stratigraphic lithology,and magmatic activity,and is a hydrothermal filling type deposit.

关键词

渑池县/重晶石矿床/地质特征/控矿因素

Key words

Mianchi county/barite deposits/geological characteristics/ore control factor

引用本文复制引用

郭钢阳,崔东豪..河南黄金山重晶石矿床地质特征与矿床成因[J].中国非金属矿工业导刊,2024,(1):66-70,5.

中国非金属矿工业导刊

OACSTPCD

1007-9386

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