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皖浙赣边界岩浆岩带区域成矿特征及成矿规律研究

余有林 陈芳 胡召齐

安徽地质2026,Vol.36Issue(1):11-14,45,5.
安徽地质2026,Vol.36Issue(1):11-14,45,5.

皖浙赣边界岩浆岩带区域成矿特征及成矿规律研究

Regional Metallogenic Characteristics and Regularities of the Anhui-Zhejiang-Jiangxi Border Igneous Belt

余有林 1陈芳 1胡召齐1

作者信息

  • 1. 安徽省地质调查院(安徽省地质科学研究所),安徽 合肥 230001
  • 折叠

摘要

Abstract

The Anhui-Zhejiang-Jiangxi border igneous belt is situated at the junction of the Yangtze and Cathaysia Plates,where tectonic and Yanshanian magmatic activities are well developed,and gold,lead-zinc,tungsten,molybdenum and other polymetallic deposits(occurrences)are widely distributed.Based on a systematic review of regional deposit types and their distribution patterns,this paper analyzes the control of strata,structures and magmatic rocks on mineralization,and explores the sources of ore-forming materials and fluids using fluid inclusion and isotopic geochemical methods.A"shear zone-magmatic hydrothermal"mineralization model is then constructed.The study suggests that mineralization is controlled by NE-trending ductile-brittle shear zones and Early Yanshanian(~141 Ma)high-K calc-alkaline granites.The main ore-forming materials are derived from deep magmatic hydrothermal fluids,with partial contributions from the assimilation of shallowly metamorphosed basement rock series.Regional mineralization exhibits a distinct zonation characterized by"structure-controlled belts,intrusion-controlled rocks,and alteration-controlled ores".This research provides a theoretical basis for the new round of mineral exploration.

关键词

皖浙赣边界/岩浆岩带/成矿特征/成矿规律/剪切带-岩浆热液模式

Key words

Anhui-Zhejiang-Jiangxi border/Igneous belt/Metallogenic characteristics/Metallogenic regularities/Shear zone-magmatic hydrothermal model

分类

天文与地球科学

引用本文复制引用

余有林,陈芳,胡召齐..皖浙赣边界岩浆岩带区域成矿特征及成矿规律研究[J].安徽地质,2026,36(1):11-14,45,5.

基金项目

中国地质调查局项目"安徽省矿产地质志"(编号:DD20221695、DD20190379、DD20160346)资助 (编号:DD20221695、DD20190379、DD20160346)

安徽地质

1005-6157

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