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松辽盆地钱家店砂岩型铀矿床含矿岩系组成特征与铀成矿作用*
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宋柏荣1, 孙慧2, 杨松林1, 韩洪斗1, 李青春3, 施玉华1, 唐洁云1, 刘玉婷1 |
Characteristics and uranium mineralization of ore-bearing rock series in Qianjiadian sandstone-type uranium deposits, Songliao Basin
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Song Bai-Rong 1, Sun Hui 2, Yang Song-Lin 1, Han Hong-Dou 1, Li Qing-Chun 3, Shi Yu-Hua 1, Tang Jie-Yun 1, Liu Yu-Ting 1
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钱家店铀矿赋矿砂岩类型微观图版 a—矿化蚀变方解石交代杂基(QⅣ-20-23,335.2 m,正交偏光);b—重晶石交代早期方解石(QⅣ-120-57,456.28 m,正交偏光); c—粒间后生氧化铁(QⅣ-41-05,332.5 m,单偏光);d—油泥痕或逸散晕圈(QIV-53-08,338.4 m,正交偏光) |
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