| 注册
首页|期刊导航|地质与勘探|河南省萤石矿床地质特征、成矿规律及找矿方向

河南省萤石矿床地质特征、成矿规律及找矿方向

白俊豪 张渐渐 孔令菲

地质与勘探2024,Vol.60Issue(3):458-470,13.
地质与勘探2024,Vol.60Issue(3):458-470,13.DOI:10.12134/j.dzykt.2024.03.002

河南省萤石矿床地质特征、成矿规律及找矿方向

Geological Characeristics,Metallogenic Regularity and Prospecting Direction of Fluorite Deposits in Henan Province

白俊豪 1张渐渐 2孔令菲3

作者信息

  • 1. 河南省国土空间调查规划院,河南郑州 450000
  • 2. 河南省第五地质大队有限公司,河南郑州 450000
  • 3. 河南省第二地质矿产调查院有限公司,河南郑州 450000
  • 折叠

摘要

Abstract

Fluorite is a strategic mineral in China.It is of great significance to improve the resource reserves of fluorite for the development of national economy.This study systematically summarized the metallogenic regularity of fluorite deposits and suggested the future prospecting direction by analyzing the geological characteristics,spatiotemporal distribution,and source of ore-forming materials of fluorite deposits in Henan Province.The results indicate that:(1)fluorites deposits in Henan Province are dominated by hydrothermal filled type,and can be divided into three fluorite metallogenic belts.(2)The fluorite deposits in Henan Province are mainly located within the Mesozoic granitic intrusions or along the surrounding NW-and NE-trending fault zones.Fluorite deposits in the Fangcheng area mainly occur in the strata near the granitic intrusions.(3)The metallogenic age of the fluorite deposits was about 120 Ma,and the fluorite deposits in the Fangcheng area may have formed in the Neoproterozoic.(4)The Mesozoic granitic magmatism or post-hydrothermal activity provided important materials and driving heat for fluorite mineralization.The rocks provided important fluorine for fluorite mineralization,and their rich calcium source may be the key to the enrichment of massive fluorite.(5)The ore-forming fluid in the main mineralization stage of fluorite should be low temperature,low salinity,and low density,and atmospheric precipitation played an important role in fluorite mineralization.(6)The key areas for fluorite exploration in Henan Province should be located in the northern belt and central belt where the Taihua Group and the Mesozoic granitic intrusions are widely developed,especially in the interior or surrounding areas of intrusions such as Heyu,Taishanmiao,Tianmushan,and Tongshan.

关键词

萤石矿床/地质特征/成矿年龄/成矿物质/成矿流体/找矿方向/河南省

Key words

fluorite deposit/geological characteristics/metallogenic age/ore-forming material/ore-forming fluid/prospecting direction/Henan Province

分类

天文与地球科学

引用本文复制引用

白俊豪,张渐渐,孔令菲..河南省萤石矿床地质特征、成矿规律及找矿方向[J].地质与勘探,2024,60(3):458-470,13.

基金项目

2021年度河南省财政地质勘查项目(编号:豫自然资发[2021]16号-12)、河南省矿产资源国情调查项目(编号:豫自然资办函[2020]22号)和2024年度河南省财政地质勘查新立项目(编号:豫财招标采购-2024-424-11)联合资助. (编号:豫自然资发[2021]16号-12)

地质与勘探

OA北大核心CSTPCD

0495-5331

访问量0
|
下载量0
段落导航相关论文