Geological Characteristics and Prospecting of Zhongjiashan Lead-zinc Mine Deposit in Fengyang of Anhui

杨本忠

doi:10.16056/j.1005-7676.2018.01.003

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Geological Characteristics and Prospecting of Zhongjiashan Lead-zinc Mine Deposit in Fengyang of Anhui

更新时间：2026-01-19

- Geological Characteristics and Prospecting of Zhongjiashan Lead-zinc Mine Deposit in Fengyang of Anhui
- Issue 1, Pages: 9-12(2018)
- 作者机构：
  
  华东冶金地质勘查研究院
- 作者简介：
- 基金信息：
- DOI：10.16056/j.1005-7676.2018.01.003
  CLC： P618.42;P618.43
- Published：2018
- 稿件说明：
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[1]杨本忠.安徽凤阳中家山铅锌矿地质特征及找矿方向[J].能源研究与管理,2018(01):9-12.

杨本忠. Geological Characteristics and Prospecting of Zhongjiashan Lead-zinc Mine Deposit in Fengyang of Anhui[J]. 2018, (1): 9-12.
[1]杨本忠.安徽凤阳中家山铅锌矿地质特征及找矿方向[J].能源研究与管理,2018(01):9-12. DOI： 10.16056/j.1005-7676.2018.01.003.

杨本忠. Geological Characteristics and Prospecting of Zhongjiashan Lead-zinc Mine Deposit in Fengyang of Anhui[J]. 2018, (1): 9-12. DOI： 10.16056/j.1005-7676.2018.01.003.

摘要

凤阳中家山铅锌矿位于华北陆块东南缘与扬子陆块衔接部位

小张庄组（Arxz）是该矿床的主要含矿地层。矿区内含矿蚀变带严格受断裂构造带控制

多形成断裂构造带、矿化蚀变带

矿化体三体一位的构造格局。中家山铅锌矿是严格受断裂构造控制

以脉状产出的构造蚀变岩型铅锌多金属矿床。构造蚀变岩带和物探激电异常-高（低）阻高级化异常是该矿的重要找矿标志。

Abstract

Zhongjiashan lead-zinc deposit is located in the southeast margin of north China continental block and Yangtze landmass join parts. Xiaozhangzhuang group（Arxz） is the main ore-bearing strata of the deposit. Mining area containing mineral alteration with strictly controlled by faulted structure belt. Formation fracture tectonic belt

the mineralization alteration belt and the mineralization body are tectonic framework of deposit. Zhongjiashan lead-zinc deposit is strictly controlled by fracture structure

with vein of tectonic altered rock type lead-zinc polymetallic deposit. Tectonic altered rock zone and geophysical anomaly-high（low） high-level resistance anomalies are important prospecting marks of the mine.

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