| 广西那坡果提金矿成因新认识 |
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| 引用本文： | 陆有德.广西那坡果提金矿成因新认识[J].南方国土资源,1999,12(4):31-34. |
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| 作者姓名： | 陆有德 |
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| 作者单位： | 广西第四地质队,广西 南宁 530030 |
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| 摘 要： | 广西那坡县果提金矿是近年化探异常查证发现、并控制了一定储量且地质特征特殊的矿床 ,矿体产于下泥盆统郁江组下部硅化压碎岩中 ,受上寒武统博莱田组碳酸盐岩古侵蚀面控制。通过矿体分布特征和形态产状、矿石特点的研究 ,认为果提金矿属岩溶沉积间断面微细粒金矿。
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| 关 键 词： | 金矿床 岩溶沉积 微细粒金矿 成因 |
| 修稿时间： | 〕：
1999-07-09 |
A NEW VIEWPOINT OF GENESIS OF GUOTI GOLD DEPOSIT IN GUANGXI NABO |
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| Authors: | LU You-de |
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| Abstract: | Guoti gold deposit is one of special features and some resesves deposit found by geochemical anomaly in spection in Guangxi Napo, The ore-body has been found in silicified cataclasite of lower Yujang formation of lower Denonian and controlled by erosion Paleo-surface of carbonate rock of upper Cambrian Bocaition formation. By studies on the distribution and attitudes of the mine, The author thought that Guoti gold deposit is a discontinuity surface of karst sedimentation of Microfinegrained gold deposit |
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| Keywords: | gold deposit karst sedimentation Micro-grained gold deposit genesis |
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