摘要
苗儿山矿田为中南地区五大铀矿田之一,其内分布有我国最大规模碳硅泥岩型的铲子坪铀矿床及诸多花岗岩型铀矿床,沙子江矿床为矿田内重要的花岗岩型铀矿床之一。沥青铀矿是理想的铀矿床直接定年样品,同时,也是U-Pb同位素研究的理想矿物。本次研究以沥青铀矿为对象进行U-Pb同位素分析,获得了沙子江矿床早、晚两期铀成矿作用的年代分别为104.4Ma和53.0±6.4Ma,结合铲子坪矿床主成矿期年代74.1±9.9Ma,它们可能分别代表了苗儿山矿田3期主要铀成矿作用的时代。沙子江矿床等时线拟合所得高的初始Pb值反映了该期成矿作用之前存在铀的预富集作用。3期成矿作用与华南地区基性脉岩年代数据统计反映的岩石圈伸展期次相对应,暗示了铀成矿受控于华南岩石圈伸展这一大的动力学环境。
Miaoershan uranium ore field, one of the five large-scale uranium ore fields in central South China, hosts the largest carbonaceous-siliceous-pelitic rock type uranium ore deposit in China-the Chanziping uranium ore deposit, along with many other granite-type uranium deposits. The Shazijiang deposit is one of important granite-type uranium deposits in the ore field. Pitchblende is not only ideal sample to date uranium mineralization directly but good mineral for measurement of U-Pb isotope testing as well. U-Pb isotope measurements of pitchblende samples from the Shazijiang uranium ore deposit in northern Guangxi of China indicate that there existed two mineralization stages, 104.4 Ma and 53.0±6.4 Ma. Combined with the major mineralization age of 74.1±9.9 Ma for the Chanziping uranium ore deposit, three major mineralization stages can be defined for the Miaoershan uranium ore field （104.4 Ma, 74.1±9.9 Ma and 53.0±6.4 Ma）. High initial Pb isotope ratio obtained by pitchblende U-Pb isochron method for the Shazijiang uranium ore deposit suggests that pre-mineralization had already occurred before this major mineralization stage. Three major mineralization stages are consistent with epochs of lithospheric extension in South China as indicated by mafic dikes geochronology, implying that uranium mineralization was constrained by the geodynamic setting of lithospheric extension.
出处
《地质学报》
EI
CAS
CSCD
北大核心
2010年第8期1175-1182,共8页
Acta Geologica Sinica
基金
国家重点基础研究发展规划项目(编号2007CB411408)
国家自然科学基金项目(编号40634020)资助成果
