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黝铜矿

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Argentite ; native silver ; polybasite ; freibergite ; lead-zinc deposit ; Guizhou

辉银矿;自然银;流锑铜银矿;银黝铜矿;铅锌矿床;贵州

In the ores there exist a low-temperature mineral assemblage of arsenopyrite, stibnite, jamesonite, silver fahlerz,berthierite, and electrum, which is consistent with the measurement result of the ore temperature. It can be seen that one the outstanding features of the Sawaya''erdun gold deposit is low-temperature metallogenesis.

在矿床中发现的一套由针状毒砂-辉锑矿-脆硫锑铅矿-银黝铜矿-辉锑铁矿-自然银-单斜磁黄铁矿等组成的低温矿物组合,与成矿温度的测定结果(主阶段100-230℃)相当吻合,显示出该矿床的成矿特殊性-低温成矿作用。

Independent silver minerals in the deposits areargentite, native silver, polybasite and freibergite, which are mainlydistributed within galena.

矿床中显微级独立银矿物有辉银矿、自然银、硫锑铜银矿和银黝铜矿,主要分布于方铅矿中。

The content of Sb has decreased from the original value of 8.3% to value of 1.02% which indicate the destruction of tetrahedrite.

锑的含量已从最初的8.3%降到1.02%的值,表明了黝铜矿的破坏。

Investigation of silver minerals in these ore deposits shows that the silver-bearing tetrahedrite and freibergite are among the most important or main industrial silver minerals.

按国际矿物学协会新矿物及矿物命名委员会的矿物命名原则,黝铜矿族矿物所含的Fe、Zn、Hg、Cd、Mn等不可作为矿物种的命名元素。

It must be pointed out that the silverbearing tetrahedrite and freibergite of the Caijiaying deposit have about the same iron and zinc content, but differ from the Fe_rich and Zn-poor tetrahedrite and freibergite in the Xiasai,Lamo, Mount Isa and Langdal deposits.

按国际矿物学协会新矿物及矿物命名委员会的矿物命名原则,黝铜矿族矿物所含的Fe、Zn、Hg、Cd、Mn等不可作为矿物种的命名元素。

The gold ores have mineral association of pyrite, tetrahedrite, chalcopyrite, galena, sphalerite and Au-Ag mineral series, and element association of Au-Cu-Ag-Pb-As-Sb-Bi, which show certain vertical zonal regularity.

矿石矿物组合为黄铁矿、黝铜矿、黄铜矿、方铅矿、闪锌矿和Au-Ag系列矿物,具Au-Cu-Ag-Pb-As-Sb-Bi的元素组合,并显示一定的垂直分带规律。其成因类型为地下热卤水型。

There is a strongly positive linear correlation between the mole numbers of antimony and silver in freibergite.

在银黝铜矿中,Ag 的摩尔数与Sb、Zn的摩尔数呈明显正相关。

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