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内蒙古大兴安岭南段敖包吐铅锌银矿床成矿机制研究

刘利宝 王祥东 王巍巍

华南地质2026,Vol.42Issue(3):509-519,11.
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华南地质2026,Vol.42Issue(3):509-519,11.DOI:10.3969/j.issn.2097-0013.2026.03.011

内蒙古大兴安岭南段敖包吐铅锌银矿床成矿机制研究

Metallogenic Mechanism of Aobaotu Lead-Zinc-Silver Deposit in Southern Great Xing'an Range,Inner Mongolia

刘利宝 1王祥东 2王巍巍3

作者信息

  • 1. 内蒙古第九地质矿产勘查开发有限责任公司,内蒙古 锡林浩特 026000||山东省地质矿产勘查开发局第六地质大队,山东 威海 264209||中国地质科学院地质研究所,北京 100037
  • 2. 中国地质调查局武汉地质调查中心(中南地质科技创新中心),湖北 武汉 430205
  • 3. 内蒙古第三地质矿产勘查开发有限责任公司,内蒙古 呼和浩特 010011
  • 折叠

摘要

Abstract

[Objective]Aobaotu Pb-Zn-Ag polymetallic deposit has been newly discovered in the great xing'an range in recent years.Previous studies have evaluated the hydrothermal vein-type ore bodies controlled by fault structures,but the mechanism of lead-zinc-silver mineralization remains unclear and requires further research.[Methods]In this study,the formation age,material sources,and genetic mechanism of the deposit are systematically investigated via zircon geochronology,in-situ S-Pb isotope analysis,and H-O isotope measurement.[Results]The results show that:(1)The ore-forming parent rock yields a formation age of 156.7±2.5 Ma,which constrains the timing of mineralization to Late Jurassic.(2)In situ sulfur isotope characteristics reflect the magma source of sulfur.The in-situ Pb isotope characteristics reflect that Pb is a mixed source of crust and mantle,and it is a kind of mineralization closely related to magmatism from crust-mantle interaction.(3)Hydrogen and oxygen isotope studies indicate that the ore-forming fluids were dominated by magmatic-hydrothermal fluids in the early stage,with the addition of meteoric water in the late stage.[Conclusions]The Aobaotu Pb-Zn-Ag deposit was formed in the Late Jurassic.Granodiorite porphyry provided the source material for Pb-Zn-Ag mineralization,and the nearly E-W-trending faults and their secondary fractures are the main ore-hosting structures.This deposit is a fracture-controlled mesothermal magmatic hydrothermal vein-type deposit,associated with regional Late Jurassic tectono-magmatic-hydrothermal activity.

关键词

成岩时代/物质来源/矿床成因/敖包吐/大兴安岭南段

Key words

Rock-forming age/Material source/Ore deposit genesis/Aobaotu/Southern Great Xing'an range

分类

天文与地球科学

引用本文复制引用

刘利宝,王祥东,王巍巍..内蒙古大兴安岭南段敖包吐铅锌银矿床成矿机制研究[J].华南地质,2026,42(3):509-519,11.

基金项目

内蒙古自治区地质勘查基金项目(项目编号:11-2-KC35、12-3-KC15) (项目编号:11-2-KC35、12-3-KC15)

华南地质

1007-3701

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