广西大瑶山西侧层控矿床成因类型及成矿机理 |
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引用本文: | 袁少平,张振贤,周怀玲.广西大瑶山西侧层控矿床成因类型及成矿机理[J].南方国土资源,1989(4). |
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作者姓名: | 袁少平 张振贤 周怀玲 |
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作者单位: | 广西石油地质队
(袁少平,张振贤),广西石油地质队(周怀玲) |
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摘 要: | 本文根据《广西大瑶山西侧泥盆系铅锌黄铁矿床控矿条件及成矿预测研究》成果,按照沉积演化观点,将本区层控矿床成固类型划分为成岩矿床、成岩—后生矿床和后生矿床。成矿物质主要来源于赋矿地层下泥盆统及基底岩石,成矿溶液主要为大气降水经深循的渗流热卤水,成矿物质的聚集与成岩后生作用有关,矿床的形成可分为沉积、成岩、后生三个阶段,并建立了成矿模式。
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关 键 词: | 铅锌矿 铜矿 黄铁矿 重晶石 层控矿床 下泥盆统 成因 广西大瑶山 |
ON THE GENETIC TYPES AND ORE-FORMING MECHANISM OF STRATA-BOUND ORE DEPOSITS IN WESTERN DAYAOSHAN MOUNTAIN, GUANGXI |
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Authors: | Yuan Shaoping Zhang Zhengxian and Zhou Huailing |
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Institution: | Petroleum Geological Party of Guangxi |
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Abstract: | This paper is based on the reseach project The Controls and Minerogenetic Prognosis of Devonian Pb-Zn-Pyrite Deposits in Western Dayaoshan, Guangxi. According to the evolution of sedimentation, the strata-bound deposits in this area can be grouped into three genetic types, ie,, diagenetic deposit and diagenetic-epigenetic deposit, and epigenetic deposit. The ore-forming materials are mainly derived from the Sipai Stage (Lower Devonian) and the basement, whereas the ore-forming solutions are hot brine produced by meteoric water Circulating deep in the earth. The enrichment of the ore-forming materials are related to epigehetic processes. The ore deposits may have formed during three stages: deposition, diagenesis, and post-diagenesis. This paper also sets up a metallogenic model for ore deposits of this type. |
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Keywords: | lead-zone ore copper ore pyrite barite strata-bound ore deposit lower Devonian genesis Dayaoshan |
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