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贺州南乡龙水脉石英矿地质特征及矿床成因浅析

魏小昭

中国非金属矿工业导刊Issue(2):32-36,70,6.
中国非金属矿工业导刊Issue(2):32-36,70,6.

贺州南乡龙水脉石英矿地质特征及矿床成因浅析

Geological Characteristics and Mineral Origin Analysis of Longshui Stone Quarry in Nanxiang,Hezhou

魏小昭1

作者信息

  • 1. 广西贺州市矿业投资集团有限公司,广西 贺州 542800
  • 折叠

摘要

Abstract

The Longshui stone quartz mine in Nanxiang,Hezhou,is located in the northeastern part of the Dabie-South China orogenic belt Guangxi central-northeastern fold and fracture system,where the Longshui Fault structure has been strictly controlling the occurrence of the quartz vein deposit].The Longshui stone quartz mine is a granite magmatic hydrothermal deposit formed by the filling and alteration of silica-rich hydrothermal fluids along the fault.This paper analyzes the main geological features and genesis of the Longshui stone quartz mine to provide a basis for subsequent mining development in the area.

关键词

脉石英/地质特征/矿床成因/贺州/广西

Key words

vein quartz/geological features/genesis of mineral deposits/Hezhou/Guangxi

分类

天文与地球科学

引用本文复制引用

魏小昭..贺州南乡龙水脉石英矿地质特征及矿床成因浅析[J].中国非金属矿工业导刊,2025,(2):32-36,70,6.

中国非金属矿工业导刊

1007-9386

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