1) paleochannel-type sandstone-hosted uranium deposit
古河道型砂岩铀矿
1.
On the base of the application of transient electromagnetic technique of paleochannel-type sandstone-hosted uranium deposits in Tengchong region of Yunan Province, This paper analyses the detect example.
可为我国其它地区的古河道型砂岩铀矿勘查提供借鉴。
3) channel sandstone type uranium deposit
河道砂岩型铀矿
1.
Analysis on depositional system and discussion on ore-formation conditions of channel sandstone type uranium deposit--taking Dongsheng area,Ordos Meso-Cenozoic basin as an example;
沉积体系分析与河道砂岩型铀矿成矿条件讨论——以鄂尔多斯中新生代盆地东胜地区为例
4) basal-channel sandstone-type uranium deposits
底河道砂岩型铀矿
1.
On the base of the deposit researching,it is concluded that basal-channel sandstone-type uranium deposits with roll front must need two conditions: the first is the metallogenic sandbody has better stratified,connectivity and permeability;the second is the stratigraphic frame must be have better water-resisti.
通过对该铀矿地质特征的研究,认识到发育卷状矿体的底河道砂岩型铀矿必须具备两大条件:其一是成矿砂体条件,即砂体要有较好的成层性、连通性和渗透性;其二是地层结构条件,即砂体必须存在较好的上、下隔水岩层。
5) paleochannel type uranium deposit
古河道型铀矿床
1.
This paper systematically introduces the geologic background,characteristics of uranium mineralization and uranium metallogenic conditions of the three regions in Russia(Transural,western Siberia and Transbaikal regions) where important paleochannel type uranium deposits have been discovered.
本文系统地介绍了俄罗斯 3个具有工业意义的古河道型铀矿化发育区 (外乌拉尔、西西伯利亚和外贝加尔 )的地质背景、铀矿化特征和铀成矿条件 ,指出切割到基底中的古河道型铀矿床 ,既可产于跨地区的造山带周围 ,也可产于活化的年青地台和古老地盾 ;既可形成于干燥的气候条件 ,也可形成于潮湿的气候条件。
6) sandstone type uranium deposit
砂岩型铀矿
1.
A method of quantitative prediction for sandstone type uranium deposit in Russia and its application;
俄罗斯砂岩型铀矿成矿定量预测技术及应用
2.
Analyses on anomaly of radon and its daughters above sandstone type uranium deposit;
砂岩型铀矿床上氡及其子体异常分析
3.
3D groundwater flow simulation in a sandstone type uranium deposit in-situ leaching field;
某可地浸砂岩型铀矿区地下水水流三维数值模拟
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