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柴达木盆地七个泉背斜狮子沟组与七个泉组构造-沉积演化及对砂岩型铀矿成矿的启示*
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施源1, 刘卫红2, 邱隆伟1, 高雪峰3, 董道涛4, 王宇喆5 |
Tectonic-sedimentary evolution of the Shizigou and Qigequan Formations in Qigequan Anticline in Qaidam Basin: implications for the mineralization of sandstone-type uranium deposits
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SHI Yuan 1, LIU Weihong 2, QIU Longwei 1, GAO Xuefeng 3, DONG Daotao 4, WANG Yuzhe 5
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七个泉背斜Y沟地层结构和沉积旋回特征(Y1至Y6露头位置见 图 2 ) |
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