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天马山硫金矿床金的赋存状肪及分布规律
引用本文:吕俊武,夏元法.天马山硫金矿床金的赋存状肪及分布规律[J].地质与勘探,2001,37(3):29-31.
作者姓名:吕俊武  夏元法
作者单位:铜陵有色金属集团公司,
摘    要:矿床中金主要以独立矿物相存在,少数为细粒分散相,金的载体矿物主要有黄铜矿,毒砂,黄铁矿,综合脉石和磁黄铁矿等,金矿物主要为自然金,银金矿,平均成色745.57,金的嵌布类型有粒间金,包裹金,裂隙金3种,金在矿石中及不同矿体中的分布不均匀,金与流,金与砷的相关性因矿体类型及矿石类型的不同而有差异。

关 键 词:赋存状态  分布规律  硫金矿床  天马山  载体矿物  黄铜矿  毒砂  包裹体  裂隙金
文章编号:0495-5331(2001)03-00 29-03
修稿时间:2000年4月10日

OCCURRENCE AND DISTRIBUTION OF GOLD IN THE TIANMASHAN SULFUR-GOLD DEPOSIT
LU Jun-wu,XIA Yuan-fa.OCCURRENCE AND DISTRIBUTION OF GOLD IN THE TIANMASHAN SULFUR-GOLD DEPOSIT[J].Geology and Prospecting,2001,37(3):29-31.
Authors:LU Jun-wu  XIA Yuan-fa
Abstract:Gold occurs mainly in mineral state. Only a small amount is in fine-grained dispersed phase. Gold-Carrying minerals are mainly chalcopyrite, arsenopyrite, pyrite, gangue, pyrrhotite and so on. Gold minerals are mainly Gold, silver-gold, the fineness averaging 745.57. Gold is embedded as inter-crystal, inclusion and fissure-filling form. Gold is uneven distributed in ores and orebodies. Correlation of Gold to sulfur, gold to arsenic depend on types of orebodies and ores.
Keywords:Occurrence state of Gold  distribution regulation  sulfur-gold deposit  Tianmashan
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