At Scinto 6 uranium occurs in much altered dolerite below the unconformity.
“辛托6”
铀矿体产于不整合面之下变质甚深粒玄岩中。
At Scinto 6 uranium occurs in much altered dolerite below the unconformity.
“辛托6”铀矿体产于不整合面之下变质甚深粒玄岩中。
Electronmicroscopic examination shows that Ti-oxide (rutile or anatase) is replaced by brannerite, indicat-ing the metasomatic origin of brannerite.
在电镜下观察到钛铀矿与钛氧化（金
锐钛矿）成交代关系，说明钛铀矿是交代成因。
Interlayer oxidized zone and argillite-sisandstone-argillite sequence occur in red clastic rock formation with ideal artesian and circulating system of ground water.
在色
屑岩建造中有层间氧化带和“泥-砂-泥”结构发育，并有良
下水承压和循环体制，是寻找可浸砂岩型铀矿有利区。
So little is known about it, because there is only about 1 ATOM OF FRANCIUM IN A CUBIC FOOT OF URANIUM ORE!
对它所知甚少,因为在1立方英尺铀矿中,仅有1个钫原子!
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