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1)  Cataclastic-alteration granite-type uranium deposit
碎裂蚀变花岗岩型铀矿
2)  granite-type uranium deposit alteration zone
花岗岩型铀矿床蚀变带
3)  Cataclastic-altered granite type
碎裂蚀变花岗岩型
1.
Cataclastic-altered granite type uranium deposit is one of the main prospecting objects inour country at present.
碎裂蚀变花岗岩型铀矿床是当前我国找矿的主攻方向之一,它具有大碎裂带、以交代作用为特征的大蚀变带。
4)  granite-type uranium deposit
花岗岩型铀矿床
1.
210Po measurements of borehole core for granite-type uranium deposit in Miaoershan area indicate that there are high and large range anomaly which greatly exceeds uranium orebody in uranium mineralization area.
在苗儿山地区已知花岗岩型铀矿床上的试验结果显示,在矿化规模较大、品位较高的钻孔岩心剖面上观察到了分布范围大大超过矿体,且强度较高的210Po异常。
2.
Thus,it is one of the main U-producing granite-type uranium deposits in South China.
302铀矿床规模大,垂幅深(达1000多米),是我国华南主要产铀花岗岩型铀矿床之一。
5)  granite type uranium deposit
花岗岩型铀矿床
1.
Ore-bearing and barren rocks and soils were sampled in granite type uranium deposits, and their glowing curves and intensities were measured.
在花岗岩型铀矿床上分别采集了含矿和无矿岩石样品及含矿和无矿土壤样品,用精密热释光剂量仪测量了它们的发光曲线和发光强度,并对所测结果进行了对比分析。
2.
The surveying results along two known profiles prove its feasibility in search for deep granite type uranium deposits.
文中简单介绍了土壤天然热释光方法的测量原理,探讨了该方法在寻找隐伏花岗岩型铀矿床中应用的可行性。
6)  granite-type uranium deposit
花岗岩型铀矿
1.
Aero-radioactive information extraction and integration for the exploration of granite-type uranium deposits
花岗岩型铀矿勘查中航放信息的提取与综合
2.
More than 86% of known granite-type uranium deposits in the study area are located within the zones with fault fractal dimension greater than 1.
研究区花岗岩型铀矿田内约有86%的铀矿床位于断裂分维值D偏高(D>1。
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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