| 砂岩型铀矿的双重还原介质模型及其联合控矿机理:兼论大营和钱家店铀矿床 |
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| 引用本文： | 焦养泉,吴立群,荣辉.砂岩型铀矿的双重还原介质模型及其联合控矿机理:兼论大营和钱家店铀矿床[J].地球科学,2018,43(2):459-474. |
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| 作者姓名： | 焦养泉 吴立群 荣辉 |
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| 作者单位： | 中国地质大学构造与油气资源教育部重点实验室, 湖北武汉 430074 |
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| 基金项目： | 中国核工业地质局高校科技攻关项目201409国家重点基础研究发展计划（"973"计划）项目子课题2015CB453003中央高校基本科研业务费专项资金G1323511660中国核工业地质局高校科技攻关项目201150国土资源部中央地质勘查基金专题研究项目2013150011中国石油辽河油田分公司重大项目LHYT-TLYK-2012-JS-8593中国石油辽河油田分公司重大项目LHYT-KTXMGLB-2010-JS-13848国土资源部铀矿整装勘查综合研究项目12120114076501国土资源部铀矿整装勘查综合研究项目12120114014301中国核工业地质局高校科技攻关项目2016026329国土资源部中央地质勘查基金专题研究项目2008150013国家自然科学基金项目41502105 |
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| 摘 要： | 含铀岩系的还原介质可以依据与铀储层砂体的产出关系划分为内部还原介质和外部还原介质.铀储层砂体的双重还原介质对铀成矿同等重要.铀储层砂体中的层间氧化作用直接与内部还原介质相关，但是当叠加有外部还原介质时，外部还原介质将通过不同的方式大大增强铀储层砂体的整体还原能力，这种组合的出现有利于稳定的层间氧化带发育和持续的铀成矿.沉积期的古气候和沉积环境决定了含铀岩系还原介质的类型和丰度，以及铀储层砂体双重还原介质的组合规律，并从根本上决定了成矿期层间氧化带的发育规模.在进行砂岩型铀矿的勘查预测时，需要将双重还原介质模型评价与具体盆地的地质背景和成矿期控矿条件研究相结合，才能获得理想的结果.
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| 关 键 词： | 还原剂 地质模型 铀储层 砂岩型铀矿 矿床学 |
| 收稿时间： | 2017-08-20 |
Model of Inner and Outer Reductive Media Within Uranium Reservoir Sandstone of Sandstone-Type Uranium Deposits and Its Ore-Controlling Mechanism: Case Studies in Daying and Qianjiadian Uranium Deposits |
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| Abstract: | The Daying and Qianjiadian uranium deposits, the reductive media within uranium-bearing series are divided into inner reductive media and outer reductive media according to its occurrence relationship with uranium reservoir sandstone. The assemblage of the inner and outer reductive media was in favor of the formation of the interlayer oxidation zone and continuous uranium mineralization. It is found that the interlayer oxidation within uranium reservoir sandstone was directly related with the inner reductive media and the reducibility of uranium reservoir sandstone was largely enhanced when the outer reductive media participated in the process of interlayer oxidation. The reductive media outside uranium reservoir sandstone was just as important to uranium mineralization as the reductive media inside uranium reservoir sandstone. Types and abundance of the reductive media inside and outside uranium reservoir sandstone and their spatial distribution were affected by the synsedimentary palaeoclimate and depositional environment of uranium-bearing series which basically constrained the scale of interlayer oxidation zone. The desired results will be achieved during prospecting prediction for the sandstone-type uranium deposit based on evaluation of the model of the double reductive media associated with the studies of geological background and ore-controlling conditions in the uranium mineralization stage. |
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