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Mineral Exploration and Resource Evaluation

Trace Element Characteristics of Zircon and Apatite Metallogenic in Rocks of Hukeng Tungsten Deposit in Western Jiangxi Province:Implications for Petrogenesis and Mineralization

  • Hua WANG , 1 ,
  • Shaohao ZOU , 1 ,
  • Long CHEN 2 ,
  • Deru XU 1 ,
  • Xilian CHEN 1 ,
  • Xuena WANG 1 ,
  • Haodong FENG 1
Expand
  • 1. State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, Jiangxi, China
  • 2. The Fourth Geological Brigade of Jiangxi Geological Bureau, Pingxiang 337000, Jiangxi, China

Received date: 2022-06-09

  Revised date: 2022-09-13

  Online published: 2023-01-06

Highlights

The South China Block is an important polymetallic metallogenic area mainly related to the W,Sn,Cu and other metals,most of that mineralization is closely related to the Mesozoic magmatism.Based on the analysis of zircon U-Pb dating and trace element of apatite and zircon of the muscovite granite related to mineralization in the Hukeng tungsten deposit,the age,magmatic properties and evolution characteristics of the metallogenic rock was constraint in this study.The results show that the muscovite granite was formed at (152.3±1.73)Ma,which is consistent with the peak period of polymetallic mineralization in South China(170~150 Ma).In addition,trace element of apatite shows that it has a M-shaped REE chondrite normalized pattern,with features of enrich in F[w(F) is 3.52%~4.09%)]and Mn(5 081×10-6~13 948×10-6),and depleted in Cl[w(Cl)<0.012%] and Mg(5.91×10-6~24.08×10-6),which are consistent with that in the high fractionated S-type granite.Besides,trace element of zircon shows that it has high Th/U ratio,LREE-depleted and HREE-enriched REE chondrite normalized pattern.Furthermore,the oxidized state and temperature of the rock were constraint by Ce,U and Ti content in zircon,which shows that zircon was crystallized at the conditions of high temperature(800 ℃) and low oxygen fugacity in the early period of magma.Combined with previous studies,it is concluded that the Hukeng granite experienced strong early fractional crystallization and the formation of the Hukeng deposit may be related to the evolution of reductive highly fractionated magmas.

Cite this article

Hua WANG , Shaohao ZOU , Long CHEN , Deru XU , Xilian CHEN , Xuena WANG , Haodong FENG . Trace Element Characteristics of Zircon and Apatite Metallogenic in Rocks of Hukeng Tungsten Deposit in Western Jiangxi Province:Implications for Petrogenesis and Mineralization[J]. Gold Science and Technology, 2022 , 30(6) : 848 -865 . DOI: 10.11872/j.issn.1005-2518.2022.06.074

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全力推进新轮找矿突破 保障国家能源资源安全

中国地质调查局矿产资源研究所近日组织召开新一轮找矿突破战略行动关键理论与技术方法研讨会。会议旨在深入学习贯彻党的二十大精神和习近平总书记给山东省地矿局第六地质大队全体地质工作者重要回信精神,梳理制约找矿突破的重大理论和关键技术难题,总结找矿理论与技术方法。

自然资源部党组成员,中国地质调查局党组书记、局长李金发,全国政协常委、中国地质调查局副局长李朋德,自然资源部科技发展司司长姚华军线上参会。中国工程院院士毛景文、中国地调局资源所所长陈仁义主持会议。

会议特别邀请了何继善、汤中立、许志琴、陈毓川、裴荣富、赵文津、多吉、孙传尧、彭苏萍、陈骏、邵安林、杨经绥、王双明、侯增谦、林君、王运敏、陈军、李献华、邓军、胡瑞忠、孙友宏等22位院士和张洪涛、王保良等专家参会。

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会议指出,新一轮找矿突破战略行动需充分发挥科技创新引领作用,聚焦制约找矿突破的重大科学问题及勘查开发利用中“卡脖子”的技术难题,实现关键理论与技术方法突破,推广运用一批绿色、适用、高效的勘查技术方法,提高矿产资源勘查技术水平。充分发挥院士专家的智囊作用,加强找矿行动业务咨询和技术指导,协助解决找矿中的疑难问题。下一步,中国地调局资源所将深入总结本次研讨成果,按照新一轮找矿突破战略行动总体部署,坚持目标导向、问题导向,聚焦主攻矿种、主攻矿床类型、重点成矿区带,梳理制约找矿突破的关键理论和技术方法,切实履行“资源报国”的使命担当,努力实现地质找矿新突破,全力服务国家能源资源安全保障。

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