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澳大利亚兰杰一号铀矿之生命周期:地质、资源、生产与修复
引用本文:林子瑜,聂逢君,张士红,徐翅翔,余倩.澳大利亚兰杰一号铀矿之生命周期:地质、资源、生产与修复[J].地质通报,2019,38(11):1867-1876.
作者姓名:林子瑜  聂逢君  张士红  徐翅翔  余倩
作者单位:东华理工大学, 江西 抚州 344000,东华理工大学, 江西 抚州 344000,中国地质科学院, 北京 100037;中国地质大学(北京), 北京 100083,东华理工大学, 江西 抚州 344000,东华理工大学, 江西 抚州 344000
基金项目:中国核工业地质局项目《铀资源大数据分析与找矿战略研究》(编号:201928-3)
摘    要:兰杰一号铀矿及其所属的鳄鱼河铀矿田产于北澳太古宙克拉通内古元古代裂谷背景下发展起来的松溪造山带,矿体产于新太古代—古元古代结晶-变质基底/晚古元古代—中元古代康博尔吉红层建造不整合界面之下,铀矿化分3个时代,U_1为1720~1680Ma,U_2为1420~1040Ma,U_3为474±6Ma,U1是主矿化时代。该矿床于1969年后期通过航空放射性测量被发现,1970’s经勘探圈定了No.1和No.3两个铀矿体,总计资源储量124681t@0.23%U_3O_8。1980年10月正式露采,至2018年12月,总计生产了128739t U_3O_8。1985财年开始,ERA(澳大利亚能源资源有限责任公司)向世界核能市场共计销售了产于兰杰铀矿的119882t U_3O_8。2009年,发现了No.3深部矿,探明资源储量为43857t@0.22%U_3O_8,这部分资源将以地下开采方式利用。预计到2026年,采区地貌景观和生态环境将得到恢复。进一步讨论了澳北元古宙不整合面型铀矿找矿的方向,持续稳定的铀矿开采与生产的意义,以及投资澳大利亚铀矿业需要注意的政治与法律问题。这些内容可以为国内矿业企业及地勘单位合理部署澳洲铀矿勘查与开发提供参考。

关 键 词:兰杰铀矿  元古宙不整合面型  核燃料  铀生产  环境修复
收稿时间:2019/5/26 0:00:00
修稿时间:2019/7/30 0:00:00

The life of Ranger 1 uranium mine in Australia: Geology, resources, production and rehabilitation
LIN Ziyu,NIE Fengjun,ZHANG Shihong,XU Chixiang and YU Qian.The life of Ranger 1 uranium mine in Australia: Geology, resources, production and rehabilitation[J].Geologcal Bulletin OF China,2019,38(11):1867-1876.
Authors:LIN Ziyu  NIE Fengjun  ZHANG Shihong  XU Chixiang and YU Qian
Affiliation:East China University of Technology, Fuzhou 344000, Jiangxi, China,East China University of Technology, Fuzhou 344000, Jiangxi, China,Chinese Academy of Geological Sciences, Beijing 100037, China;China University of Geosciences(Beijing), Beijing 100083, China,East China University of Technology, Fuzhou 344000, Jiangxi, China and East China University of Technology, Fuzhou 344000, Jiangxi, China
Abstract:The tectonic setting of Ranger uranium deposit, also ARUF, is Pine Creek orogen, which was developed from the Paleoproterozoic rift in the Archean craton of North Australia. The orebodies lie under the interface between the Neoarchaean-Paleoproterozoic crystallization-metamorphic basement and Late Paleo-Mesoproterozoic Kombolgie red bed formations. There are three epochs of uranium mineralization, which are U1:1720~1680Ma, U2:1420~1040Ma and U3:474±6Ma. U1 is the main mineralization epoch.The deposit was discovered by aerial radioactivity survey in late 1969. No. 1 and No. 3 orebodies were delineated by exploration in the 1970''s, with a total resource of 124681t@0.23% U3O8. From October 1980 to December 2018, a total of 128739t U3O8 was produced by open-pit mining. Since fiscal year 1985, ERA has sold 119882t U3O8 from Ranger uranium mine to the nuclear energy market in the world. In 2009, No. 3 deep orebody was discovered, with reserves of 43857t@0.22% U3O8, which will be exploited by underground mining. It is expected that the geomorphological landscape and ecological environment of the mining area will be restored by 2026.This paper further discusses the prospecting direction of Proterozoic unconformity uranium deposits in northern Australia, the significance of sustained and stable uranium mining and production, and the political and legal issues that need attention in investing in Australian uranium mining. These contents can provide references for China''s mining enterprises and geological exploration units to rationally deploy Australian uranium exploration and development.
Keywords:Ranger uranium mine  Proterozoic unconformity  nuclear fuel  uranium production  environmental rehabilitation
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