| 注册
首页|期刊导航|世界有色金属|东至县花山地区金矿体特征及金的成因探讨

东至县花山地区金矿体特征及金的成因探讨

钟光杰 郑磊 杜志正

世界有色金属Issue(12):96-98,3.
世界有色金属Issue(12):96-98,3.

东至县花山地区金矿体特征及金的成因探讨

Discussion on the characteristics of gold deposits and the genesis of gold in the Huashan area of Dongzhi County

钟光杰 1郑磊 1杜志正1

作者信息

  • 1. 安徽省地质矿产勘查局324地质队,安徽 池州 247100
  • 折叠

摘要

Abstract

The tectonic position of the Huashan gold mine area is located in the southern part of the Jiangnan transition zone,on the south side of the Jiangnan deep fault,and from the east to the west side of the fault.The ore body is controlled by nearly east-west trending faults,and the ore bearing rocks are the early Cambrian Yangliugang Formation striped mudstone and clay shale.The main ore minerals are pyrite,arsenopyrite,antimonite,etc.Among them,granite diorite porphyry pyrite mineralization is developed,sericite mineralization is developed,and is accompanied by more common vein disseminated gold mineralization,which has the characteristics of porphyry type gold deposits.In the Jiangnan transition zone,medium acidic porphyry should be the focus of searching for porphyry type gold deposits.The indicators for mineral exploration include structure,lithology,and alteration.

关键词

花山/金矿/条纹灰岩/细脉浸染状

Key words

Huashan/Gold mines/Striped limestone/Fine vein impregnation

分类

天文与地球科学

引用本文复制引用

钟光杰,郑磊,杜志正..东至县花山地区金矿体特征及金的成因探讨[J].世界有色金属,2024,(12):96-98,3.

世界有色金属

1002-5065

访问量0
|
下载量0
段落导航相关论文