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我国砂岩型铀矿成矿构造研究现状及发展趋势OA

Research status and development trend of sandstone-type uranium deposit metallogenic structures in China

中文摘要英文摘要

[研究目的]传统砂岩型铀矿成矿理论在构造控矿作用方面存在认识局限,而我国砂岩型铀矿床的分布与产出特征明显受构造控制.为深入解析构造要素对铀成矿过程的制约机制,文章对我国主要砂岩型铀矿集区的成矿特征进行系统研究,旨在揭示不同构造背景下铀成矿作用的差异表现及其成因.[研究方法]通过对我国西北、中北及东北部典型砂岩型铀矿集区的成矿特征开展综合对比分析,结合成矿动力学背景,探讨构造—流体—成矿之间的耦合关系.[研究结果]研究表明,西北地区铀成矿作用集中于挤压造山带前陆盆地环境,形成典型的层间氧化带型铀矿床;中北部地区则表现出与走滑断裂系统密切相关的复合型成矿特征;东北地区铀矿化主要受伸展构造体制控制,发育深部热流体叠加改造型铀矿化.深部流体沿断裂系统运移并改变含矿层地球化学环境,促进铀在有利构造部位聚集成矿;新构造运动通过断裂再活化与盆地差异隆升等过程,不仅改造先存矿化体,还形成多期次流体叠加成矿的复杂特征.[结论]构造驱动下的表生—深部流体成矿机制是理解砂岩型铀矿成矿规律的关键.建议今后重点构建构造—流体—成矿耦合模型,并加强深部找矿预测技术的应用,为铀资源勘查拓展新领域提供理论和技术支撑.

[Objective]The traditional theory of sandstone-type uranium mineralization has limitations in understanding the role of tectonics in mineralization.However,the distribution and occurrence characteristics of sandstone-type uranium deposits in China are significantly controlled by tectonics.To deeply analyze the constraining mechanism of tectonic elements on the uranium mineralization process,we systematically study the mineralization characteristics of the main sandstone-type uranium deposit clusters in China,aiming to reveal the different manifestations and causes of uranium mineralization under different tectonic backgrounds.[Method]By conducting a comprehensive comparative analysis of the mineralization characteristics of typical sandstone-type uranium deposit clusters in Northwest,North Central and Northeast China,and combining the mineralization dynamic background,the coupling relationship between tectonics,fluids,and mineralization is explored.[Results]The study shows that uranium mineralization in Northwest China is concentrated in the foreland basins of compressive orogenic belts,forming typical interlayer oxidation zone-type uranium deposits;in North Central China,it exhibits complex mineralization characteristics closely related to strike-slip fault systems;uranium mineralization in Northeast China is mainly controlled by the extensional tectonic regime,with the development of deep thermal fluid superimposed and remodeled uranium mineralization.Deep fluids migrate along fault systems and alter the geochemical environment of ore-bearing layers,promoting the accumulation of uranium in favorable tectonic positions;neotectonic movements,through the reactivation of faults and differential uplift of basins,not only transform pre-existing mineralization bodies but also form complex features of multi-stage fluid superimposed mineralization.[Conclusion]The coupling mechanism of tectonics,fluids,and mineralization is the key to understanding the mineralization laws of sandstone-type uranium deposits.It is suggested that in the future,efforts should be focused on constructing a coupling model of tectonics,fluids,and mineralization,and strengthening the application of deep exploration prediction technologies to provide theoretical and technical support for expanding the exploration of uranium resources.

封志兵;佘尚阳;白磊;张鑫;李立尧;江丽;齐增硕;史佳乐;王晓菲

东华理工大学核资源与环境国家重点实验室,江西南昌 330013||中国地质调查局天津地质调查中心(华北地质科技创新中心),天津 300170东华理工大学核资源与环境国家重点实验室,江西南昌 330013中国石油长庆油田分公司工程造价部,西安,710018东华理工大学核资源与环境国家重点实验室,江西南昌 330013东华理工大学核资源与环境国家重点实验室,江西南昌 330013东华理工大学核资源与环境国家重点实验室,江西南昌 330013东华理工大学核资源与环境国家重点实验室,江西南昌 330013东华理工大学核资源与环境国家重点实验室,江西南昌 330013东华理工大学核资源与环境国家重点实验室,江西南昌 330013

天文与地球科学

砂岩型铀矿控矿构造成矿作用新构造运动地震勘探

sandstone-type uranium depositore-controlling structuresmineralization processneotectonic movementsseismic exploration

《华北地质》 2025 (4)

1-16,16

中国地质调查局华北地质科技创新中心人才培育基金项目(2024HBPJ-Q09)、中国铀业有限公司-东华理工大学核资源与环境国家重点实验室联合创新基金项目(2023NRE-LH-08)、江西省自然科学基金项目(20252BAC240270)、国家自然科学基金项目(U2244205)资助成果 Supported by the Talent Cultivation Fund Project of the North China Geological Science and Technology Innovation Center of the China Geological Survey(2024HBPJ-Q09),the Joint Innovation Fund Project of China Uranium Industry Co.,Ltd.East China University of Technology-State Key Laboratory of Nuclear Resources and Environment(2023NRE-LH-08),the Natural Science Foundation Project of Jiangxi Province(20252BAC240270),and the National Natural Science Foundation Project(U2244205).

10.19948/j.12-1471/P.2025.04.01

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