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黄铁矿

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Fine- grain native gold and electrum occur in the major gold -carrying minerals like quartz, native bismuth, bismuthinite, pyrrhotite, pyrite, chalcopyrite and araenopyrite at the state of interlocking, inter- granular, crevice and enclosure.

金矿物以形态复杂的微粒、细粒自然金、银金矿、金银矿为主,赋存形式有晶隙金、包体金、连生金、裂隙金,载金矿物为石英、自然铋、辉铋矿、磁黄铁矿黄铁矿、黄铜矿、毒砂等。

The main ore minerals are chalopyrite、bornite、chalopyrite、pyrite and nature silver, are mineral zoned from redbed to graybed appear chalcocite、bornite、 chalcopyrite and pyrite, chalcocite occur in front of ore bodies.

矿石矿物主要为辉铜矿、斑铜矿、黄铜矿、黄铁矿和自然银,很少见闪锌矿和方铅矿。矿物分带明显,从红层、辉铜矿、斑铜矿、黄铜矿、黄铁矿到浅色层,辉铜矿形成于矿体的前锋。

Based on the relationship between properties of chalcopyrite and pyrite and their flotability, the new technology of instant flotation for chalcopyrite and pyrite has been studied in this paper.

本文根据黄铜矿、黄铁矿的性质与可浮性的关系,研究了黄铜矿、黄铁矿快速浮选分离的新技术。

The disseminated blebs are generally composed of one pyrrhotite individual accompanied by varying amounts of pentandite and chalcopyrite.

分散的泡体常由磁黄铁矿个体与多少不等的镍黄铁矿及黄铜矿共生。

A new dressing technology, selective flotation separation of gold, and flotation separating pyrite from arsenopyrite with chlorinated lime as the oxidizing agent, and magnetic separation of pyrrhotite from arsenopyrite is adopted and good beneficiation indexes are achieved.

天马山矿矿石属含砷高硫难选金矿石,对该矿石进行了选矿工艺研究,采用优先浮选金、漂白粉作氧化剂氧化浮选分离黄铁矿和毒砂、磁选分离磁黄铁矿和毒砂工艺,综合回收金硫砷,取得较好选别指标。

Minor element discrimination indices for residual primary sulfides (pyrite, pyruhotite, chalcopyrite, sphalerite, galena, etc.) and supergene ore minerals goethite, hematite, manganiferons minerals, covellite, native gold, clay minerals, quartz, etc.

还给出了残余原生硫化物(黄铁矿、磁黄铁矿、黄铜矿、闪锌矿、方铅矿等)和表生矿物(针铁矿、赤铁矿、锰矿物、铜蓝、自然金、粘土矿物、石英等)的微量元素评价标志。

The investigation on depressant s of pyrrhotite at home and abroad is reviewed in this paper.

本文概括了与磁黄铁矿浮选电化学有关的几个方面的研究情况和国内外对磁黄铁矿抑制剂的研究概况。

The morphology of these grains reveals that the iron sulfides originated from the eluvium loam above hypothetical ore deposits in the vicinity of the section or glaciofluvial sediments from nearby glacial margins.

磁性矿物颗粒的形貌特征进一步揭示Znojmo地区黄土/古土壤所含黄铁矿或磁黄铁矿主要由附近源区搬运而来,冰缘沉积物和周围台地的风化剥蚀物是黄土物质的主要来源。

The sulfide mineral mainly consists of pyrite, and a small amount of pyrrhotite, galena and sphalerite.

硫化矿矿物主要为黄铁矿,其次为少量的磁黄铁矿、方铅矿、闪锌矿。

Both pyrrhotite and pentlandite are also oxidized by Fe(superscript 3+) besides direct bio-oxidation.

黄铁矿氧化时间大致是其他两种矿物的3倍,因而工业配矿可酌量降低富含黄铁矿之金精矿用量。

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