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桂北摩天岭岩体舒家湾地区沥青铀矿原位微区年代学及其地质意义

刘明 谭双 陈琪 范鹏飞 万建军 吴昆明 朱小兵 雷勇亮

铀矿地质2025,Vol.41Issue(4):617-636,20.
铀矿地质2025,Vol.41Issue(4):617-636,20.DOI:10.3969/j.issn.1000-0658.2025.41.043

桂北摩天岭岩体舒家湾地区沥青铀矿原位微区年代学及其地质意义

In Situ Microchronology and Geological Significance of Pitchblende in Shujiawan Area of Motianling Pluton,Northern Guangxi

刘明 1谭双 1陈琪 1范鹏飞 1万建军 2吴昆明 1朱小兵 1雷勇亮1

作者信息

  • 1. 核工业二三〇研究所,湖南 长沙 410007||湖南省伴生放射性矿产资源评价与综合利用工程技术研究中心,湖南 长沙 410007
  • 2. 东华理工大学 铀资源探采与核遥感全国重点实验室,江西 南昌 330013
  • 折叠

摘要

Abstract

Shujiawan area is located in the northern part of the Motianling pluton,characterized by numerous uranium mineralization occurrences,anomaly points,diverse ore-bearing fractures,and bears significant metallogenic potential.To precisely determine the uranium mineralization age in the study area,this study conducted chemical composition analysis,U-Pb isotopic dating,and rare earth element(REE)characterization of pitchblende using in-situ microanalysis techniques(EPMA,LA-ICP-MS)based on optical microscopy and scanning electron microscopy backscatter observations.Results show that the mass fraction of pitchblende is of UO2(87.56%average),CaO(1.21%),PbO(0.58%),and P2O5(0.78%).The 206Pb/238U weighted average age was determined as(54.5±1.5)Ma(MSWD=2.2,n=16),while the Tera-Wasserburg concordia diagram yielded a lower intercept age of(55.0±1.5)Ma(MSWD=2.2,n=16).Both ages are consistent within error limit,indicating a mineralization age of approximately 55 Ma.REE characteristics of pitchblendes reveal relatively low total REE contents with insignificant LREE-HREE fractionation,but distinct negative Eu anomalies.The chondrite-normalized REE pattern displays a V-shaped curve with slight LREE enrichment and relatively flat HREE distribution.The ΣREE contents,ThO2 and Y concentrations,and Eu anomalies collectively indicate a low-temperature hydrothermal origin with corresponding fluid characteristics.The obtained mineralization age corresponds to the 45-55 Ma lithospheric extension period in South China and mate with the critical uranium mineralization period(87-47 Ma)during Late Yanshanian to Early Himalayan brittle-ductile extensional tectonic activities in Motianling structural dome.This demonstrates that uranium mineralization in Shujiawan area was formed under a Cretaceous-Paleogene lithospheric extension and thinning geodynamic background,representing a product of late-stage uranium mineralization events in South China.

关键词

LA-ICP-MS U-Pb同位素定年/沥青铀矿/成矿时代/舒家湾地区

Key words

LA-ICP-MS U-Pb dating/pitchblende/metallogenic age/Shujiawan area

分类

天文与地球科学

引用本文复制引用

刘明,谭双,陈琪,范鹏飞,万建军,吴昆明,朱小兵,雷勇亮..桂北摩天岭岩体舒家湾地区沥青铀矿原位微区年代学及其地质意义[J].铀矿地质,2025,41(4):617-636,20.

基金项目

中国核工业地质局地勘项目(编号:202223、202222) (编号:202223、202222)

核工业二三〇研究所自主研发/创新创效项目(编号:2022-02-09) (编号:2022-02-09)

江西省研究生创新基金(编号:YC2023-B208)联合资助. (编号:YC2023-B208)

铀矿地质

1000-0658

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