Yongjian Wang , Kezhang Qin , Honghai Fan , Yaqing Pang
{"title":"复杂热液铀矿系统中铀矿U[sbnd]Pb时计稳健性评价——来自华南象山火山相关铀矿田的启示","authors":"Yongjian Wang , Kezhang Qin , Honghai Fan , Yaqing Pang","doi":"10.1016/j.chemgeo.2025.123058","DOIUrl":null,"url":null,"abstract":"<div><div>Accurate dating of hydrothermal uranium deposits has long been challenging due to the complex alteration of uranium minerals such as uraninite, which complicates the interpretation of U<img>Pb isotopic data. This study addresses this issue by presenting new U<img>Pb dating results from uraninite in the Xiangshan volcanic-related uranium ore field, South China, using in situ LA-ICP-MS. Through detailed petrographic observations and elemental scanning, we carefully selected well-preserved uraninite grains/veins that were minimally affected by post-mineralization alteration. The uraninite U<img>Pb geochronology yields the precise and reliable <sup>208</sup>Pb-corrected U<img>Pb age of 137.0 ± 4.5 Ma and <sup>204</sup>Pb-corrected U<img>Pb age of 139.1 ± 4.7 Ma, respectively, demonstrating remarkable consistency with the coeval hydrothermal apatite U<img>Pb age (ca. 135 Ma) obtained from the same hand specimen. Petrographic and elemental mapping analyses show that Pb-bearing minerals are commonly distributed as tiny particles along the microfractures or within the margins of the altered uraninite grains. This heterogeneity of Pb distribution is likely a result of fluid-aided modification induced by post-ore tectono-thermal events, which causes isotopic resetting and Pb loss, leading to inaccurate or misleading U<img>Pb ages. In addition, the presence of a large amount of anomalous Pb-bearing minerals (e.g., Pb-bearing molybdenum sulfide, pyrite) within the uraninite samples can also lead to younger-than-expected U<img>Pb ages. More importantly, the new mineralization age is, within error, nearly identical to the volcanic rock emplacement ages. This close temporal match, coupled with the geochemical signature of the uraninite, strongly suggests a genetic link between volcanic magmatism and uranium mineralization, indicating the Xiangshan uranium ore field might be formed during a short but continuous mineralization event rather than through a protracted and complex sequence of mineralization episodes. Additionally, this study highlights the need for careful interpretation of uraninite U<img>Pb dates in geologically complex uranium or uranium-associated ore systems.</div></div>","PeriodicalId":9847,"journal":{"name":"Chemical Geology","volume":"695 ","pages":"Article 123058"},"PeriodicalIF":3.6000,"publicationDate":"2025-09-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Assessing the robustness of uraninite UPb chronometer in complex hydrothermal uranium ore systems: Insights from Xiangshan volcanic-related uranium ore field, South China\",\"authors\":\"Yongjian Wang , Kezhang Qin , Honghai Fan , Yaqing Pang\",\"doi\":\"10.1016/j.chemgeo.2025.123058\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Accurate dating of hydrothermal uranium deposits has long been challenging due to the complex alteration of uranium minerals such as uraninite, which complicates the interpretation of U<img>Pb isotopic data. This study addresses this issue by presenting new U<img>Pb dating results from uraninite in the Xiangshan volcanic-related uranium ore field, South China, using in situ LA-ICP-MS. Through detailed petrographic observations and elemental scanning, we carefully selected well-preserved uraninite grains/veins that were minimally affected by post-mineralization alteration. The uraninite U<img>Pb geochronology yields the precise and reliable <sup>208</sup>Pb-corrected U<img>Pb age of 137.0 ± 4.5 Ma and <sup>204</sup>Pb-corrected U<img>Pb age of 139.1 ± 4.7 Ma, respectively, demonstrating remarkable consistency with the coeval hydrothermal apatite U<img>Pb age (ca. 135 Ma) obtained from the same hand specimen. Petrographic and elemental mapping analyses show that Pb-bearing minerals are commonly distributed as tiny particles along the microfractures or within the margins of the altered uraninite grains. This heterogeneity of Pb distribution is likely a result of fluid-aided modification induced by post-ore tectono-thermal events, which causes isotopic resetting and Pb loss, leading to inaccurate or misleading U<img>Pb ages. In addition, the presence of a large amount of anomalous Pb-bearing minerals (e.g., Pb-bearing molybdenum sulfide, pyrite) within the uraninite samples can also lead to younger-than-expected U<img>Pb ages. More importantly, the new mineralization age is, within error, nearly identical to the volcanic rock emplacement ages. This close temporal match, coupled with the geochemical signature of the uraninite, strongly suggests a genetic link between volcanic magmatism and uranium mineralization, indicating the Xiangshan uranium ore field might be formed during a short but continuous mineralization event rather than through a protracted and complex sequence of mineralization episodes. Additionally, this study highlights the need for careful interpretation of uraninite U<img>Pb dates in geologically complex uranium or uranium-associated ore systems.</div></div>\",\"PeriodicalId\":9847,\"journal\":{\"name\":\"Chemical Geology\",\"volume\":\"695 \",\"pages\":\"Article 123058\"},\"PeriodicalIF\":3.6000,\"publicationDate\":\"2025-09-16\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Chemical Geology\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0009254125004486\",\"RegionNum\":2,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Chemical Geology","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0009254125004486","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
Assessing the robustness of uraninite UPb chronometer in complex hydrothermal uranium ore systems: Insights from Xiangshan volcanic-related uranium ore field, South China
Accurate dating of hydrothermal uranium deposits has long been challenging due to the complex alteration of uranium minerals such as uraninite, which complicates the interpretation of UPb isotopic data. This study addresses this issue by presenting new UPb dating results from uraninite in the Xiangshan volcanic-related uranium ore field, South China, using in situ LA-ICP-MS. Through detailed petrographic observations and elemental scanning, we carefully selected well-preserved uraninite grains/veins that were minimally affected by post-mineralization alteration. The uraninite UPb geochronology yields the precise and reliable 208Pb-corrected UPb age of 137.0 ± 4.5 Ma and 204Pb-corrected UPb age of 139.1 ± 4.7 Ma, respectively, demonstrating remarkable consistency with the coeval hydrothermal apatite UPb age (ca. 135 Ma) obtained from the same hand specimen. Petrographic and elemental mapping analyses show that Pb-bearing minerals are commonly distributed as tiny particles along the microfractures or within the margins of the altered uraninite grains. This heterogeneity of Pb distribution is likely a result of fluid-aided modification induced by post-ore tectono-thermal events, which causes isotopic resetting and Pb loss, leading to inaccurate or misleading UPb ages. In addition, the presence of a large amount of anomalous Pb-bearing minerals (e.g., Pb-bearing molybdenum sulfide, pyrite) within the uraninite samples can also lead to younger-than-expected UPb ages. More importantly, the new mineralization age is, within error, nearly identical to the volcanic rock emplacement ages. This close temporal match, coupled with the geochemical signature of the uraninite, strongly suggests a genetic link between volcanic magmatism and uranium mineralization, indicating the Xiangshan uranium ore field might be formed during a short but continuous mineralization event rather than through a protracted and complex sequence of mineralization episodes. Additionally, this study highlights the need for careful interpretation of uraninite UPb dates in geologically complex uranium or uranium-associated ore systems.
期刊介绍:
Chemical Geology is an international journal that publishes original research papers on isotopic and elemental geochemistry, geochronology and cosmochemistry.
The Journal focuses on chemical processes in igneous, metamorphic, and sedimentary petrology, low- and high-temperature aqueous solutions, biogeochemistry, the environment and cosmochemistry.
Papers that are field, experimentally, or computationally based are appropriate if they are of broad international interest. The Journal generally does not publish papers that are primarily of regional or local interest, or which are primarily focused on remediation and applied geochemistry.
The Journal also welcomes innovative papers dealing with significant analytical advances that are of wide interest in the community and extend significantly beyond the scope of what would be included in the methods section of a standard research paper.