流体包裹体在东胜砂岩铀矿成矿研究中的应用
pplication of Fluid Inclusions to the Research of Sandstone-type Uranium Deposit
还原作用一直被认为是许多砂岩铀矿床铀沉淀的主要机理。对于油、气、煤和铀等多种能源矿产富集的鄂尔多斯盆地,东胜铀矿的主要还原剂可能是油、气、煤中的一种或多种。通过系统的有机岩石学及流体包裹体分析表明:砂岩铀矿层中仅存在极少量镜煤和亮煤细条带,显微镜下观测到包裹体类型以气液包裹体为主,少见油包裹体,因此排除了煤和石油是东胜铀矿的还原剂的可能性。油包裹体丰度(GOI主体小于1);同时结合区域地质条件及邻区中生界地层成熟度处于临界成熟(0.40%~0.55VRo),不存在倾油性源岩,证明液态烃不是铀成矿的主要还原剂。砂岩铀矿碳酸盐胶结物碳氧同位素较轻,说明东胜直罗组砂岩铀矿起还原作用主要是富含CH4等还原性气体的天然气。
he reduction explains the main mechanism of the precipitation of uranium mineral bed. Dongsheng sandstone-type uranium deposit’s reducing agents can be one of oil, gas, coal and uranium or some of them. Systematic study of organic petrology and testing of gas inclusion indicates that: in the formation of sandstone uranium only exist a few vitrain or clarain bands, and the inclusions were mainly gas-liquid fluid inclusions with minor oil fluid inclusions. Therefore, Dongsheng sandstone-type uranium deposit’s reducing agents can not be coal or oil. The frequency of grains containing oil inclusions (GOI) are less than 1% in most of the samples, the maturity of Mesozoic Stratum is been in critical mature status (0.40%~0.55VRo), and there are not oil source rocks around Dongsheng sandstone-type uranium deposit. Also, liquid hydrocarbons are not the uranium deposit’s reducing agents. Tracing of inclusion’s hydrogen and oxygen stable isotopes of carbonate cement and lower C-O isotopes indicate that, the main reducing agents for uranium mineralization of Dongsheng sandstone-type uranium deposit are organic hydrocarbon gas, which is rich in organic hydrocarbon gas such as CH4.
缪卫东、陈开远、张志琳
核燃料、核燃料生产地质学矿业工程理论与方法论
流体包裹体,东胜砂岩铀矿,还原剂,鄂尔多斯盆地
Fluid inclusionDongsheng sandstone-type uranium depositReducing agentOrdos basin
缪卫东,陈开远,张志琳.流体包裹体在东胜砂岩铀矿成矿研究中的应用[EB/OL].(2008-02-02)[2025-08-16].http://www.paper.edu.cn/releasepaper/content/200802-30.点此复制
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