相山铀矿田超临界流体铀成矿作用的试验初探OA
Preliminary Study on Supercritical Fluid Uranium Mineralization in Xiangshan Ore Field by High Temperature and High Pressure Experiment
相山铀矿田是中国著名的超大型火山岩型铀矿田,其铀成矿作用一直是研究的焦点和热点.前人相继提出过多种成矿理论和观点,都隐含铀成矿作用存在高温、高压阶段.随着研究程度的深入,越来越多的证据显示该矿田存在高温成矿阶段,即超临界流体作用阶段.为进一步揭示相山铀矿田铀超常富集机制,文章从超临界流体作用角度进行研究,通过富铀矿石-H2O体系、富铀矿石-NaCl-H2O体系和富铀矿石-NaHCO3-H2O体系的溶解试验,测量在流体相变过程中的铀溶解度,总结铀溶解度在相变过程中的变化特征;结合前人对矿田成矿特征、控矿因素等研究成果,初步揭示相山铀矿田超临界流体铀成矿作用,为完善热液型铀矿成矿理论和指导深部勘查提供依据.研究结果显示:富铀矿石-H2O体系、富铀矿石-NaCl-H2O体系和富铀矿石-NaHCO3-H2O体系超临界区的铀溶解度显著增高,富铀矿石-NaHCO3-H2O体系中的铀溶解度明显高于富铀矿石-H2O、富铀矿石-NaCl-H2O体系中的铀溶解度,证实CO2组分的加入有利于成矿流体萃取铀和迁移铀;超临界流体相变形成的气体富含铀,远高于常规溶液蒸汽的铀含量,证实超临界铀成矿流体相变可以形成富铀热液和富铀气体;相山铀矿田为超临界流体铀成矿作用所形成.相山矿田超临界流体铀成矿作用过程主要为超临界流体从矿源区活化萃取矿质、从矿源区至富集区迁移矿质和在富集区跨越临界点发生相变而铀析出富集成矿等3个过程,且存在相分离气体铀矿化.
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.
胡志华;林锦荣;王勇剑;王文全
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
地质学
超临界流体铀成矿作用溶解试验铀溶解度相山铀矿田
supercritical fluiduranium mineralizationdissolution experimenturanium solubilityXiangshan uranium ore field
《铀矿地质》 2025 (3)
434-447,14
国家重点研发计划项目(编号:2017YFC0602600)国家自然科学基金面上项目(编号:41573051)核材料技术创新中心基金项目(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.
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