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富磷矿三阶段动态成矿模式:黔中开阳式高品位磷矿成矿机制*
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张亚冠1, 杜远生1, 陈国勇2, 刘建中2, 陈庆刚3, 赵征4, 王泽鹏3, 邓超5 |
Three stages dynamic mineralization model of the phosphate-rich deposits: Mineralization mechanism of the Kaiyang-type high-grade phosphorite in central Guizhou Province
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Zhang Ya-Guan 1, Du Yuan-Sheng 1, Chen Guo-Yong 2, Liu Jian-Zhong 2, Chen Qing-Gang 3, Zhao Zheng 4, Wang Ze-Peng 3, Deng Chao 5
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黔中开阳地区震旦系陡山沱组磷矿床古地理演化与动态沉积成矿过程(据 王泽鹏等,2016 ; 张亚冠等,2016 ;修改) a—陡山沱组沉积早期(a矿层沉积期)黔中地区岩相古地理与剖面分析;b—陡山沱组沉积中期(夹层沉积期)黔中地区岩相古地理与剖面分析;c—陡山沱组沉积晚期(b矿层沉积期)黔中地区岩相古地理与剖面分析;d—陡山沱组沉积末期(顶板段沉积期)黔中地区岩相古地理与剖面分析 |
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