1) uranium mineralization
铀成矿带
1.
Ore-bearing horizon of uranium mineralization belt in south Qinling mainly exist in Diebu Group,Zhouqu Group and Bailongjiang Group of Silurian system.
南秦岭铀成矿带含铀层位主要是志留系迭部群、舟曲群、白龙江群,总体为一套海相碳硅泥岩建造。
2) Gan-Hang uranium metallogenic belt
赣-杭铀成矿带
3) Nanling uranium metallogenetic belt
南岭铀成矿带
4) silicalite
金-铜-铀成矿带
5) uranium metallogenesis
铀成矿
1.
Some problems concerning relationship between Mesozoic-Cenozoic lithospheric extension and uranium metallogenesis in South China;
华南地区中生代以来岩石圈伸展及其与铀成矿关系研究的若干问题
2.
Relationship between oil-gas trap and uranium metallogenesis at northern Ordos basin;
油气圈闭与鄂尔多斯盆地北部铀成矿关系探讨
6) uranium mineralization
铀成矿
1.
The discussion on the relationship between high-resolution sequence stratigraphy and uranium mineralization of Zhiluo Formation in Dongsheng area,Ordos basin;
鄂尔多斯盆地东胜地区直罗组高分辨率层序地层与铀成矿关系探讨
2.
Lithofacies characteristics of ore-hosting horizon and its relationship to uranium mineralization in Qianjiadian uranium deposit,Songliao basin;
松辽盆地钱家店铀矿床含矿层位的岩相特征及其与铀成矿的关系
3.
The main reason resulting in the difference of uranium mineralization is due to the different g.
岩石成因类型不同是造成上述杂岩体中不同地段铀成矿差异的主要原
参考词条
补充资料：铀铵铀矿
分子式：NH4)2(UO2)2(PO4)2·6H2O
CAS号：
性质：又称钙铀云母。铀矿物名，含铀54.46%。四方晶系，晶体呈四方板状，集合体呈玫瑰状、苔藓状或皮壳状。外观为瓶绿至浅绿色透明固体，有玻璃光泽，相对密度3.7。在紫外线照射下发淡黄绿色中强荧光。是少见的表生铀矿物。
CAS号：
性质：又称钙铀云母。铀矿物名，含铀54.46%。四方晶系，晶体呈四方板状，集合体呈玫瑰状、苔藓状或皮壳状。外观为瓶绿至浅绿色透明固体，有玻璃光泽，相对密度3.7。在紫外线照射下发淡黄绿色中强荧光。是少见的表生铀矿物。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。