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相山铀矿田超临界流体铀成矿作用的试验初探

胡志华 林锦荣 王勇剑 王文全

铀矿地质2025,Vol.41Issue(3):434-447,14.
铀矿地质2025,Vol.41Issue(3):434-447,14.DOI:10.3969/j.issn.1000-0658.2025.41.030

相山铀矿田超临界流体铀成矿作用的试验初探

Preliminary Study on Supercritical Fluid Uranium Mineralization in Xiangshan Ore Field by High Temperature and High Pressure Experiment

胡志华 1林锦荣 2王勇剑 2王文全2

作者信息

  • 1. 核工业北京地质研究院,北京 100029||中核集团地热勘查技术研究中心,北京 100029
  • 2. 核工业北京地质研究院,北京 100029||铀资源探采与核遥感全国重点实验室,北京 100029||中核集团铀资源勘查与评价技术重点实验室,北京 100029
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摘要

Abstract

Xiangshan uranium ore field is a famous ultra large volcanic rock type uranium ore field in China,and its uranium mineralization has always been a focus and hotspot of research.Previous scholars have proposed various mineralization theories and viewpoints,all of which suggest or imply the existence of uranium mineralization under high-temperature and high-pressure.With the deepening of research,more and more evidence shows that the ore field has a high-temperature mineralization stage,namely the supercritical fluid action stage.To further reveal the mechanism of abnormal uranium enrichment in Xiangshan ore field,this paper conducted a research from the perspective of supercritical fluid action.Through dissolution experiments in the rich uranium ore-H2O system,rich uranium ore-NaCl-H2O system,and rich uranium ore-NaHCO3-H2O system,the solubility of uranium during fluid phase transition was testified,and the variation characteristics of uranium solubility during phase transition were summarized.Based on the research results of previous studies on the mineralization characteristics and controlling factors of ore fields,the supercritical fluid uranium mineralization in Xiangshan ore field was preliminarily revealed,providing a basis for improving the theory of hydrothermal uranium mineralization and guiding deep exploration.The research results show that:The uranium solubility in the supercritical region of the rich uranium ore-H2O system,rich uranium ore-NaCl-H2O system,and rich uranium ore-NaHCO3-H2O system is significantly increased;The uranium solubility in the rich uranium ore-NaHCO3-H2O system is significantly higher than that in the rich uranium ore-H2O and rich uranium ore-NaCl-H2O systems,confirming that the addition of CO2 component is beneficial for the extraction and migration of uranium by ore-forming fluids;The gas formed by the phase transition of supercritical fluid is rich in uranium,much higher than the uranium content of conventional solution steam,confirming that the phase transition of supercritical uranium ore-forming fluid can form uranium rich hydrothermal solution and uranium rich gas;The Xiangshan uranium ore field was formed by supercritical fluid uranium mineralization.The process of supercritical fluid uranium mineralization in Xiangshan ore field mainly involves three processes:activation and extraction of minerals from the source area by supercritical fluid,migration of minerals from the source area to the enrichment area,and uranium precipitation and enrichment of minerals by crossing the critical point in the enrichment area.There is phase separation gas uranium mineralization.

关键词

超临界流体/铀成矿作用/溶解试验/铀溶解度/相山铀矿田

Key words

supercritical fluid/uranium mineralization/dissolution experiment/uranium solubility/Xiangshan uranium ore field

分类

天文与地球科学

引用本文复制引用

胡志华,林锦荣,王勇剑,王文全..相山铀矿田超临界流体铀成矿作用的试验初探[J].铀矿地质,2025,41(3):434-447,14.

基金项目

国家重点研发计划项目(编号:2017YFC0602600) (编号:2017YFC0602600)

国家自然科学基金面上项目(编号:41573051) (编号:41573051)

核材料技术创新中心基金项目(编号:地CXZX1901) (编号:地CXZX1901)

中国核工业地质局铀矿地质科研项目(编号:202446-1)联合资助. (编号:202446-1)

铀矿地质

1000-0658

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