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1)  uranium ore-formation
铀成矿过程
1.
Computer simulation engine and its application to uranium ore-formation simulation;
计算机模拟引擎及其在铀成矿过程模拟中的应用研究
2)  mineralizing process
成矿过程
1.
This paper summarized the concerned application results of the REE in the metallogeny research,coming to point that REE has an extensive application in many fields: the source of mineralizing material,the tracer in the mineralizing process and the evolution of mineralizing fluid,distinguishing the mineralizing .
在总结稀土元素在矿床学研究中的应用基础上,阐述了稀土元素在成矿物质来源、成矿过程和成矿流体演化示踪、成矿类型和成矿种属判别以及找矿标志确定等方面的应用。
3)  ore-forming process
成矿过程
1.
Mechanism of uranyl ion adsorbing and complexing onto low-rank coal and ore-forming process of uranium associated coal measures
低煤级煤与UO_2~(2+)的吸附络合及亲煤型铀矿成矿过程
4)  metallogenic process
成矿过程
1.
The metallogenic process is such that in extensional tectonic setting,submarine exhalation-sedimentation occurs,the ophiolite breaks up,exhalative materials emplace in the ultra-basic rock along fault belt and extract large mount of Cobalt element from ultra-basic rock.
其成矿过程为:在拉张环境下,蛇绿岩破碎,同时发生了海底喷流—沉积作用,喷流物质沿蛇绿岩中的构造破碎带喷出与沉积,并萃取了超基性岩中大量的钴,矿体形成后又经历了构造变位。
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
补充资料:铀铵铀矿
分子式:NH4)2(UO2)2(PO4)2·6H2
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。

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