1) uranium metallogenetic province
铀成矿省
1.
The region is located in the east of the southern edge of east-Asia crust and classified into fivesecond-class tectonic units and four uranium metallogenetic provinces according to the features of itsgeology,geophysical-chemical field and uranium mineraliztion and the difference of crust evolution-movement history.
该区位于东亚壳体南段东邵，据其地质、地球物理化学场和铀矿化特征，以及地壳演化－运动历史的差异，划分为５个二级构造单元和４个铀成矿省。
2) Uranium province
铀矿省
3) 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
4) 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
5) uranium source for ore-formation
成矿铀源
6) uranium metallogenic domains
铀成矿域
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。
参考词条