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伏廖古岩溶体地质特征及铀成矿远景分析

Geological features of palaeokarst and prospective analysis on uranium ore formation in Fuliao
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摘要 古岩溶理论找矿方法是一种新的找矿方法。广西壮族自治区古岩溶成矿条件优越。伏廖地区古岩溶体发育范围大、古岩溶堆积物有一定规模,铀成矿地质条件良好,目前已有较好的铀矿化显示。作为桂西南寻找碳硅泥岩型铀矿床的重点区域,伏廖Ⅱ号古岩溶体所在区域为铀的成矿远景区域,值得进一步工作。 Prospecting methods of palaeokarst theory is a new kind of prospecting method. The ore- forming condition on palaeokarst in Guangxi Zhuang Automonous Region is believed to be very good. Palaeokarst in Fuliao area has large development range, high rock maturities and good uranium ore- forming geological condition. Favorable uranium mineralization has already been discovered. As an important region for exploring carbonate-silicous-pelitic rock uranium deposit in the westsouth of Guangxi Zhuang Automonous Region, the region where Fuliao palaeokarst No. II located is believed to be the best uranium prospective region, which deserves further work.
机构地区 广西 广西
出处 《世界核地质科学》 CAS 2013年第3期143-147,共5页 World Nuclear Geoscience
关键词 古岩溶体 地质特征 铀成矿 远景认识 palaeokarst geological feature uranium ore-formation prospective recognition
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  • 1闵茂中,地质论评,1987年,33卷,4期,53页
  • 2王清河.373矿床成因新议与找矿[J]中国岩溶,1988(S2).
  • 3闵茂中,孔令福.论马鞍肚铀矿床与(古)岩溶的成因关系[J]地质论评,1987(04).

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