The studied blind uranium deposit is a large granite-hosted deposit typical of the metallogenic province in South China.
所研究的矿床为一个大型隐伏铀矿床，是华南铀成矿区一个典型的花岗岩型铀矿床。
These typomorphlc peculiarities of microlitic quartz can be used to study vertical zoning and localize the erosion surface of the blind uranium deposit.
微晶石英标型特征的这些差异可以作为研究隐伏铀矿床垂直分带的有效手段，并可用于判断其侵蚀截面。
It is considered that ore bodies buried deeply in iron-uranium type uranium deposit in Archean greenstone belt, have many blind ore bodies, the prospecting potential is very great.
并认为太古宙绿岩带铁-铀型铀矿矿体埋藏深、隐伏性强、盲矿体多，潜在的找矿前景相当可观。
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