桂西北MS金矿区岩石地球化学异常特征 |
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引用本文: | 农毅平.桂西北MS金矿区岩石地球化学异常特征[J].南方国土资源,1989(4). |
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作者姓名: | 农毅平 |
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作者单位: | 广西地质研究所 |
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摘 要: | 本文通过对MS微粒浸染型金矿点进行了剖面和面积的岩石地球化学测量,及其结果并进行统计分析研究,认为该矿点具有如下特征:As—Sb—Hg—Au异常组合赋存于中三叠统百逢组中段砂页岩中,与层间破碎带有关; Hg、Sb异常较弱,As、Au异常较强且吻合,表明AS、Au异常是近矿异常。实践证明,该法具有较好的找矿效果,据初步评价认为可望找到一个中型规模的金矿床。
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关 键 词: | 金矿 岩石地球化学 异常特征 微粒浸染型金矿床 |
CHARACTERISTICS OF ROCK GEOCHEMICAL ANOMALIES IN THE MS GOLD DISTRICT,NORTHWESTERN GUANGXI |
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Authors: | NongYiping |
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Institution: | Guangxi Institute of Geology |
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Abstract: | This paper is based on the study of the data obtained by profile and area rock geochemical survey in the MS micro-grained gold district in Northwestern Guangxi. The result of the study shows that the gold district has the following geochemical characteristics:
(1) As-Sb-Hg-Au anomalies occur in the sandstone and shale of the Beifeng Formation (Middle Triassic) adjacant to the major fault, and is linked to inter formational crust zones;
(2) Hg and Sb anomalies are low in intensity while As and Au anomalies are higher and show better coincidence (this usually indicates that the As and Au anomalies are near orebody) .
From the result of this study it can be seen that the discovery of a gold deposit of medium size is expectable, and that the geochemical methods employed proved to be effective in gold exploration. |
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Keywords: | gold micro-grained disseminated deposit rock geochemistry characteristics of anomaly |
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