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斑铜矿

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The effect of various factors on leaching, the catalysis of Ag〓 to chalcopyrite and bornite and the catalysis of FeS〓 to chalcopyrite were investigated.

考察了各种因素对细菌浸出效果的影响以及Ag〓对黄铜矿和斑铜矿、FeS〓对黄铜矿的催化作用。

To the pure mineral of chalcopyrite and bornite, the bioleaching research was carried out with original bacterial and domesticated bacterial.

针对单矿物黄铜矿、斑铜矿,采用原始菌和驯化菌进行了生物提取的基础研究。

The chemical phase and optical micrography analysis showed that the leaching of copper oxide could be finished soon, chalcocite and bornite could be diges.

化学物相和光学显微图像分析表明,氧化铜的浸出很快就可完成,辉铜矿和斑铜矿也以较快的速度降解为蓝辉铜矿和铜蓝,而铜蓝的浸出反应比较缓

Chalcocite and bornite are the main industrial minerals.

主要工业矿物为辉铜矿、斑铜矿

The testing results show that the average Mohs hardness of the samples is up to 4.45 and the average density is up to 2.7485 g/cm^3, where the major mineral is sericite with small scaly structure and orientational arrangement, and the other minerals are quartz, chlorite and a small quantity of zircon, orthoclase, kaolinite and bornite, etc.

测试结果表明:样品的平均摩氏硬度为4.45,平均密度为2.7485g/立方公分;其主要矿物为绢云母,呈细小鳞片状结构,定向排列,还含有石英、绿泥石以及少量的锆石、正长石、高岭石和斑铜矿等。

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。

Tianlu copper deposit which formed by foreland basin in Paleozic era is marine sandshale copper deposit,copper ore mainly is silstone type and in cludes six natural type, which are chalcocite ore, chalcocitebornite ore, bornite ore, chalcopyrite bornite ore, chalcopyrite, pyrite-chalcopynite.

摘 要:天鹿铜矿床是前陆盆地古生代海相砂页岩型铜矿,铜矿石主要为粉砂岩型,包括辉铜矿矿石、辉铜矿斑铜矿矿石、斑铜矿矿石、黄铜矿斑铜矿矿石、黄铜矿矿石、黄铁矿黄铜矿矿石6种自然类型。

Species of metallic deposits are quite complicated: Besides commonly-seen pyrite ,chalcopyrite and bornite, there exist varied copper-bismuth sulfosalt minerals(sandber}erite, Bi-tennantite, Bi-tetrahedrite, aikinite, wittichenite),tungsten-tin sulfidesand polymetallic sulfides.

金属矿物种类复杂,除常见的黄铁矿、黄铜矿、斑铜矿外,还有多种铜铋硫盐矿物(锌砷黝铜矿、铋砷黝铜矿、铋锑黝铜矿、针硫铋铅矿、硫铋铜矿)、钨锡硫化物(硫铁锡铜矿、硫钨锡铜矿)及多金属硫化物。

The ages, natures and tectonic environments of the Bangong Co porphyry copper belt have been preliminarily determined through a study of ore-bearing porphyries in the Dobuzha and Garqiong porphyry copper deposits in the porphyry copper belt.

通过对藏西班公湖斑岩铜矿带多不杂和尕尔穷2个大、中型斑岩铜矿床含矿斑岩的研究,初步查明了该铜矿带的形成时代、含矿斑岩性质及成矿构造环境。

A brownish - bronze,lustrous copper ore with the composition Cu5FeS4that tarnishes to purple when exposed to air.

斑铜矿一种棕铜或亮铜矿Cu5FeS4,含有当暴露于空气时会变成紫色的化合物

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