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浙江诸暨芙蓉山破火山口东缘萤石矿床控矿构造特征研究

仲泽 吴义 梅宏涛 储书武 黎学标 刘贤森 苏小强

安徽地质2026,Vol.36Issue(2):100-104,5.
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安徽地质2026,Vol.36Issue(2):100-104,5.

浙江诸暨芙蓉山破火山口东缘萤石矿床控矿构造特征研究

Study on the Ore-controlling Structural Characteristics of Fluorite Deposits at the Eastern Margin of the Furongshan Caldera,Zhuji,Zhejiang

仲泽 1吴义 1梅宏涛 1储书武 1黎学标 1刘贤森 1苏小强1

作者信息

  • 1. 浙江省有色金属地质勘查院 绍兴市地质矿产与地质科技重点实验室,浙江 绍兴 312000
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摘要

Abstract

The Furongshan caldera is located in the Zhuji-Yiwu area of Zhejiang Province,at the junction of the Jiangshan-Shaoxing suture zone and the Lishui-Ningbo deep fault,within the northwestern segment of the southeastern Zhejiang volcanic belt.Circular and radial faults are well-developed around the caldera,with numerous dykes intruding along the circular fault systems.This study focuses on the structural relationship between fluorite deposits and the eastern margin of the Furongshan caldera,systematically analyzing the structural control characteristics of the fluorite mineralization.Research results indicate that the fluorite deposits are primarily controlled by the circular and radial faults of the Furongshan caldera,with a formation age of the Late Cretaceous,closely linked to regional volcanic activities.In this area,analogous ore-controlling structures are widely developed,providing favorable metallogenic conditions and significant exploration potential for fluorite deposits.Notably,fluorite exhibits symbiotic or associated relationships with polymetallic minerals,offering a new perspective for regional polymetallic deposit exploration.

关键词

浙江诸暨/破火山口/萤石矿床/断裂构造/燕山期

Key words

Zhuji,Zhejiang/Caldera/Fluorite deposit/Fault structure/Yanshanian period

分类

天文与地球科学

引用本文复制引用

仲泽,吴义,梅宏涛,储书武,黎学标,刘贤森,苏小强..浙江诸暨芙蓉山破火山口东缘萤石矿床控矿构造特征研究[J].安徽地质,2026,36(2):100-104,5.

基金项目

浙江省自然资源科技项目"浙江仙居盆地萤石成矿规律研究与成矿预测"(编号:2025ZJDZ012)和"芙蓉山破火山东缘铜金多金属矿床成矿物质来源及找矿方向研究"(编号:浙自然资厅函[2024]548号)资助 (编号:2025ZJDZ012)

安徽地质

1005-6157

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