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山东省平邑县归来庄金矿物质组分及矿床成因分析
引用本文:金隆裕,沈昆.山东省平邑县归来庄金矿物质组分及矿床成因分析[J].山东国土资源,1995(1).
作者姓名:金隆裕  沈昆
作者单位:地矿部山东省中心实验室,山东省地质科学研究所
摘    要:归来庄金矿,Au是唯一达到工业品位的组分。属贫硫氧化型金矿。矿石矿物近50种之多,其中金属矿物以褐铁矿为主。金矿物有自然金、银金矿、碲铜金矿、碲金银矿,并含银矿物和极少的碲化物。金矿物粒径多<0.01mm,属细粒—微粒型金矿,其嵌连关系以粒间金为主。蚀变作用为气—热蚀变和褐铁矿化。矿床系多期多阶段矿化作用形成。为中温热液矿床。隐爆角砾岩为导矿构造,而热液侵入角砾岩是容矿构造。


ORE COMPOSITION AND GENESIS OF THE GUILAIZHUANG GOLD DEPOSIT IN PINGYI SHANDONG PROVINCE
Jin Longyu and ShenKun.ORE COMPOSITION AND GENESIS OF THE GUILAIZHUANG GOLD DEPOSIT IN PINGYI SHANDONG PROVINCE[J].Land and Resources in SHANDONG Province,1995(1).
Authors:Jin Longyu and ShenKun
Abstract:Guilaizhuang gold deposit belougs to the sulphurpoor oxidation type one in which gold is theoniy component to have reached the economic(industrial)grade. There are nearly fifty kinds ofminerais in The ore among which limonite is the predominant metallic mineral while native gold,electrum,koslovite and petzite are gold-bearing minerals In addition,there are silver-mineralsand trace amount of tellurides. Grain size of the gold minerals is commonly less than 0. 01 mm;therefore,the gold deposit belongs to the f...
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