广西隆林县隆或金矿的地质特征和成因分析 |
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引用本文: | 张振贤,吴均贵,曾广海.广西隆林县隆或金矿的地质特征和成因分析[J].南方国土资源,1996(4). |
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作者姓名: | 张振贤 吴均贵 曾广海 |
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作者单位: | 广西地质研究院,广西地球物理勘察院 |
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摘 要: | 隆林县隆或金矿属微粒型金矿,具有多层位、层状矿体为主、矿石和矿物成分简单、沉积结构构造特征,属典型层控矿床。矿床成因与生物礁的消失、滑塌事件、深水火山碎屑硅泥质上超盆地的叠覆、以及有机质的热解和分异有关。火山作用提供金的来源,火山~碎屑~浊积岩相为矿源层和含矿层,并受沉积盆地的关闭和开启影响,形成成岩矿床、成岩~后生或后生矿床
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关 键 词: | 隆或 生物礁 上超盆地 浊积岩 有机质 |
GEOLOGICAL CHARACTERISTICS AND GENETIC ANALYSIS OF GOLD DEPOSIT AT LONGHUO IN GUANGXI |
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Authors: | Zhang Zhenxian |
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Institution: | Zhang Zhenxian (Guangxi Geological Institute) Wu Jungui & Zeng Guanghai (Guangxi Geophysical Prospecting Institute) |
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Abstract: | The gold deposit at Longhuo in Guangxi belongs to micro-grained type gold deposit. The gold orebodies occur as bed in poly-horizons. The compositions of gold ore and minerals are simple and the ore is of sedimentary texture and structure. So the deposit is a typical strata-bound ore deposit. Its genesis is associated with the disappearance of biological reef, slump events, the superposition of deep-water pyroclastic siliceous and argillaceous basins, the thermal dissolution and differentiation of organic materials. The gold comes from volcanism. The source beds and ore-bearing beds are volcanic-clastic-turbidite lithofacies, and are influenced by the close and open of sedimentary basin to form diagenetic, diagenetic-epigenetic, or epigenetic ore deposit. |
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Keywords: | honghuo biological reef superimposed basin turbidite organic material |
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