新疆哈图金矿地质地球化学特征及其成矿作用  

Geological and geochemical characteristics and mineralization of Ha-Tu Gold Deposit in Xinjiang

作　　者：刘鹏鹗[1] 

机构地区：[1]长春地质学院

出　　处：《黄金》1995年第9期2-6,共5页Gold

摘　　要：哈图金矿产于特定的地质地球化学背景之上，受断裂构造及中酸性侵入岩控制。各时代地层及其组成岩石的金元素及相关元素含量低（金元素的浓集系数小于０．８），中酸性侵入岩金元素丰度值较高，断裂构造中金元素的含量最高。岩体－断裂－矿体三者是地质成矿作用的统一体。矿体中成矿元素具有垂直分带性。矿体的延深有大于延长的趋势。哈图金矿局岩浆期后中温热液矿床。Ha-Tu Gold Deposit,which is strictly controlled by faulted zone and neutral-acid intrusions,occurs on a cerium geological and geochemical background.The gold and its related elements are depleted in all strata and stratum-composing rocks of different eras (concentration factor of gold<0.8).However,the gold elements are enriched in neutral-acid intrusions and highly concentrated in faulted structure.Fracture, intrusion and orebody act as a whole in mineralhation.There is a tendency that orebodys depth is great6r than its length. Ha-Tu Gold Deposit is a postmagmatic mesothermal deposit.

关 键 词：断裂构造 中酸性侵入岩体 地球化学场 金矿 

分 类 号：P612[天文地球—矿床学] P59[天文地球—地质学]