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大兴安岭成矿带南段大座子山铜多金属矿成矿时代及其地质意义

唐昆 林淞 康志宏 陈辉 俞炳 张军成 扈德峰 王永彬

地质与勘探2024,Vol.60Issue(6):1095-1104,10.
地质与勘探2024,Vol.60Issue(6):1095-1104,10.DOI:10.12134/j.dzykt.2024.06.001

大兴安岭成矿带南段大座子山铜多金属矿成矿时代及其地质意义

Metallogenetic Epoch of the Dazuozishan Cu-Polymetallic Deposit in the Southern Part of the Great Hinggan Range Metallogenic Belt and Its Geological Significance

唐昆 1林淞 2康志宏 2陈辉 3俞炳 3张军成 4扈德峰 4王永彬2

作者信息

  • 1. 中国有色金属工业昆明勘察设计研究院有限公司,云南 昆明 650051
  • 2. 云南大学,云南省地球系统科学重点实验室,云南 昆明 650500
  • 3. 中国地质调查局发展研究中心,北京 100037
  • 4. 赤峰锐能矿业有限公司,内蒙古赤峰 024050
  • 折叠

摘要

Abstract

The Dazuozishan deposit in Inner Mongolia is a recently discovered Cu-polymetallic deposit in the southern part of the Great Hinggan Range metallogenic belt.The orebodies in this deposit occurred in the rhyolite of Upper Jurassic Manketouebo Group,and the mineralization process was divided into three stages,i.e.,white quartz-minor sulfide stage(pyrite)stage,smoky quartz-polymetallic sulfide(pyrite,sphalerite,galena,chalcopyrite and molybdenite)stage and calcite-sulfide stage(pyrite,sphalerite and galena).This work conducted Re-Os dating of six molybdenite samples from the quartz-polymetallic sulfide mineralization stage,and obtained 134.4 to 136.9 Ma of model age with a weighted average age of 135.5±0.8 Ma.These ages are consistent with the 187Re-187Os isochronous age of 136.2±3.2 Ma.It is indicated that the Dazuozishan Cu-polymetallic deposit was formed in the Early Cretaceous,which was different from the previous age constrained by the Manketouebo rhyolite.Moreover,the Re content of the molybdenite ranged from 44.31×10-6 to 92.93×10-6,plotted between the crustal and mantle source regions.It is inferred that the ore-forming materials were derived from mixed crustal and mantle source.Based on the regional tectonic and magmatic evolution,the Dazuozishan copper polymetallic deposit was formed under extensional setting triggered by joint interactions between post-orogenic continental collapse of the Mongol-Okhotsk Ocean,and retreat and rollback of the Paleo-Pacific Ocean slab.

关键词

辉钼矿/Re-Os定年/成矿时代/早白垩世/大座子山铜多金属矿/大兴安岭成矿带

Key words

molybdenite/Re-Os dating/metallogenetic epoch/Early Cretaceous/Dazuozishan Cu-polymetallic deposit/Great Hinggan Range metallogenic belt

分类

天文与地球科学

引用本文复制引用

唐昆,林淞,康志宏,陈辉,俞炳,张军成,扈德峰,王永彬..大兴安岭成矿带南段大座子山铜多金属矿成矿时代及其地质意义[J].地质与勘探,2024,60(6):1095-1104,10.

基金项目

国家自然科学基金(编号:42162009)、云南省基础研究计划项目-重点项目(编号:202201AS070004)和中地调研项目(编号:[2023]34)联合资助. (编号:42162009)

地质与勘探

OA北大核心CSTPCD

0495-5331

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