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广西隆林县隆或金矿的地质特征和成因分析
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).
作者姓名:张振贤  吴均贵  曾广海
作者单位:广西地质研究院,广西地球物理勘察院
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

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
Authors:Zhang  Zhenxian
Institution:Zhang Zhenxian (Guangxi Geological Institute) Wu Jungui & Zeng Guanghai (Guangxi Geophysical Prospecting Institute)
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.
Keywords:honghuo  biological reef  superimposed basin  turbidite  organic material
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