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唯一的矿石矿物为晶质铀矿。Uraninite is the only ore mineral.

提出该岩体晶质铀矿复成因的证据。Evidence shows that the uraninite is of polygenesis.

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在下庄铀矿田中首次发现了晶质铀矿与白钨矿的共生矿体。It is the first time to find scheelite and uraninite paragenetic orebody in Xiazhuang uranium ore field.

这种矿床的晶质铀矿是从花岗岩浆分异出来的富铀岩浆中结晶而成的。Uraninite in this type of deposit is crystallized by U-rich magma which is differentiated from granitic magma.

以浸染扶晶质铀矿形式产于混合岩中的铀矿化是华南一种新的铀矿化类型。The uranium mineralization occurs in migmatite in the form of disseminated uraninite is a new type found in south China.

花岗岩的副矿物组合类型不同,晶质铀矿的产出特点以及某些矿物学特征也存在差异。The occurrence and mineralogy features of uraninite change along with the association types of accessory minerals in granite.

尤其有一部分具有胶状构造外表特征的沥青铀矿样品的各项参数均与晶质铀矿一样。Particularly part of pitchblende samples with colloidal structure features have the same physical and optical features as uraninite.

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本文阐述珠光岩体中晶质铀矿的物理化学特征、产出位置和共生组合。Described in this paper are the physicochemical characteristics, occurrence, locality and paragenesis of uraninite in the Zhuguang mass.

认为它主要是岩浆阶段结晶的,自变质与他变质作用也产生了一些晶质铀矿。It crystallizedmainly at the magma stage, while a certain part of uraninite resultedfrom autometamorphism and all chemical metamorphism.

原生型矿床中主要铀矿物是晶质铀矿,改造型矿床中的主要铀矿物是沥青铀矿和残余的晶质铀矿。The principal uranium mineral in the deposits of primary subtype is uraninite, but in reworked subtype are pitchblende and relict uraninite.

脂铅铀矿一种由桔红到黄灰色的多种铀氧化物、硅酸盐和盐的混和物,在铀矿物的自然。An orange-red to grayish yellow mixture of several uranium oxides, silicates, and salts occurring naturally in the oxidation and hydration of uraninite.