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稀有金属矿物微区同位素定年与示踪

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作为战略性关键金属矿产资源,钨、锡、铌、钽、锂、铍、铷、铯、锆、铪、稀土等稀有金属,在国民经济与国家安全方面有着重要的研究意义.稀有金属矿石矿物微区同位素定年与示踪,是开展稀有金属矿床成矿作用研究的最直接手段,具有整体分析无可比拟的优点.近年来,钨锡铌钽锆铪稀土等稀有金属矿物微区U-Pb定年与Sr-Nd-Hf同位素示踪发展迅速,而锂铍铷铯等稀有金属矿物微区Rb-Sr/Lu-Hf定年正蓬勃发展.本文综述了黑钨矿、白钨矿、锡石、铌钽矿(铌钽氧化物类矿物的简称)、独居石、磷钇矿、氟碳铈矿等稀有金属矿物微区U-Pb定年与Sr-Nd-Hf同位素示踪技术主要进展,展望了锂云母、铁锂云母、铯沸石、钾长石(天河石)等微区Rb-Sr定年与磷钇矿、磷灰石、褐帘石、独居石、黑钨矿、白钨矿等微区Sm-Nd和Lu-Hf定年的广阔前景,获得如下认识:(1)低铀矿物U-Pb定年,除了采用高灵敏度磁式等离子质谱外,元素成像技术能很好地揭示微量元素之间相关性,进而快速锁定高U/Pb区域,提高低铀矿物U-Pb定年成功率;(2)铌钽矿-锡石激光微区Hf同位素能够直接示踪花岗岩-伟晶岩稀有金属成岩成矿物质源区,但这方面工作仍需进一步加强;(3)碰撞/反应池等离子质谱的出现,使高Rb/Sr、Sm/Nd或高Lu/Hf比矿物的同位素定年成为现实,是未来稀有金属激光微区同位素年代学发展的新方向;(4)实验方法研发与标准物质研制相辅相成、相互促进,仍是当前迫切需要解决的关键技术难题.随着战略性关键金属日渐成为国内外成矿作用研究的热点,钨锡铌钽锂铍铷铯锆铪稀土等稀有金属矿物微区同位素定年与示踪方法研究,必将为我国新一轮稀有金属矿床学研究做出应有的学术贡献.
In-situ isotopic dating and tracing of the rare-metal minerals in ore deposit
As strategic key metal mineral resources,rare metals such as tungsten,tin,niobium,tantalum,lithium,beryllium,rubidium,cesium,zirconium,hafnium and Rare Earth Elements(REEs),have important research significance in the national economy and national security.The in situ isotopic dating and tracing of rare metal ore minerals are the most direct means for conducting research on the mineralization of ore deposits,and have unparalleled advantages in bulk analysis.In recent years,the U-Pb dating and Sr-Nd-Hf isotope tracing of rare metal minerals such as tungsten,tin,niobium,tantalum,zirconium and hafnium have developed rapidly,while the Rb-Sr/Lu Hf dating of rare metal minerals such as lithium,beryllium,rubidium,cesium is thriving.This article reviews the main progress in in situ U-Pb dating and Sr-Nd-Hf isotope tracing methods for rare metal minerals such as wolframite,scheelite,cassiterite,columbite-group minerals,monazite,xenotime and bastnaesite.It also looks forward to the in situ Rb-Sr dating of rare metal minerals such as(iron,cesium)zinnwaldite,lepidolite,pollucite,potassium feldspar(Tianhe stone),as well as xenotime,apatite,allanite,monazite and wolframite of the broad prospects of Lu Hf dating for microanalysis.The conclusions have been recognized as follows:(1)In addition to using high sensitivity of SF-ICP-MS,combined with elemental imaging,U-Pb dating of low U minerals can not only reveal the correlation between trace elements,but also quickly lock in high U/Pb regions,significantly improving the success of U-Pb dating of low U minerals;(2)The in situ Hf isotope of columbite-group minerals,and cassiterite can directly trace the source area of rare metal diagenetic minerals in granite pegmatite,and this work urgently needs to be further strengthened;(3)The emergence of collision/reaction ICP-MS has made isotope dating of minerals with high Rb/Sr or high Lu/Hf ratios a reality,and is a new direction for the future development of rare metal for in situ geochronology;(4)The establishment and development of techniques and reference materials complement and promote each other,and are also key technical challenges that urgently need to be addressed.Strategic key metals have become a hot topic in the study of mineralization both domestically and internationally.The study of microanalysis isotopic dating and tracing methods for rare metal minerals such as tungsten,tin,niobium,tantalum,lithium,beryllium,rubidium,cesium,zirconium,hafnium and REEs will undoubtedly make academic contributions to the new round of rare metal deposit research in China.

Rare metal mineralsMicroanalysisIsotopic dating and tracingU-Pb/Rb-Sr/Lu-Hf geochronology

杨岳衡、吴石头、车旭东、杨明、黄超、王浩、杨进辉、王汝成、吴福元

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中国科学院地质与地球物理研究所,岩石圈演化国家重点实验室,北京 100029

南京大学内生金属矿床成矿机制研究国家重点实验室,南京大学地球科学与工程学院,南京 210023

浙江大学海南研究院,三亚 572025

稀有金属 微区分析 同位素定年与示踪 U-Pb/Rb-Sr/Lu-Hf年代学

国家重点研发计划国家自然科学基金岩石圈演化国家重点实验室自主项目

2018YFA070260042173034SKL-Z202304

2024

岩石学报
中国矿物岩石地球化学学会,中国科学院地质地球物理研究所

岩石学报

CSTPCD北大核心
影响因子:2.74
ISSN:1000-0569
年,卷(期):2024.40(4)
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