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石城县楂山里萤石矿床地质特征及成因探讨

阙兴华 庄贤贵 冯卫东 张青

中国非金属矿工业导刊Issue(1):52-55,4.
中国非金属矿工业导刊Issue(1):52-55,4.

石城县楂山里萤石矿床地质特征及成因探讨

Geological Characteristics and Genesis of Zhashanli Fluorite Deposit in Shicheng County

阙兴华 1庄贤贵 1冯卫东 1张青1

作者信息

  • 1. 江西省地质矿产勘查开发局赣南地质调查大队,江西赣州 341000
  • 折叠

摘要

Abstract

Zhashanli is a super large fluorite deposit discovered in the middle part of Wuyishan metallogenic belt in recent years,This paper analyzes and discusses the geological characteristics and genesis of the deposit in detail,thus implies that Zhashanli fluorite deposit belongs to low-middle temperature epithermal filling deposit,the orebody attitude,shape and size are controlled by fracture structure.The ore-forming materials come from wall rock and deep magrnatic hydrothermal,and the ore-forming fluid is provided by atmospheric precipitation.

关键词

萤石矿/地质特征/矿床成因/楂山里

Key words

fluorite deposit/ore characteristics/ore genesis/Zhashanli

分类

天文与地球科学

引用本文复制引用

阙兴华,庄贤贵,冯卫东,张青..石城县楂山里萤石矿床地质特征及成因探讨[J].中国非金属矿工业导刊,2017,(1):52-55,4.

中国非金属矿工业导刊

OACSTPCD

1007-9386

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