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闪锌矿

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The main mineral in the ore is marmites, pyrrhonist and arsenopyrite, rich in silver, gallium, germanium, indium and other rare metals.

摘 要:原矿中的主要金属矿物是铁闪锌矿、磁黄铁矿和毒砂,富含银、镓、锗、铟等稀贵金属。

This is because that the sample occur a transition of zinc blende structure to rocksalt structure.

导致金属化现象的本质是纳米晶发生了从闪锌矿到岩盐矿的压致结构相变。

Zinc sulfate was produced in process of soaking blende with sulfuric acid of high concentration in oxygen and at normal pressure.

研究了在常压、通氧条件下,用浓硫酸浸取闪锌矿制取硫酸锌时酸浸条件对锌浸取率的影响。

The results show that these particles are cubical zinc blende, and the morphology of raw material has little influence on the morphology of product.

结果表明,原料的形貌对产物的形貌基本没有影响,纳米硫化锌颗粒为结晶良好的立方体闪锌矿;透射电镜分析晶体的生长过程表明,晶体呈棱柱体形,遵从碱性溶液中晶体极性生氏机制。

The pressure-induced structural transition from the Zinc blende to a rocksalt phase occurs at about 12.6 GPa, and at the transition point the relative volume reduction is close to 13%.

发现样品在12.6GPa附近存在一个从立方闪锌矿型到立方岩盐矿型的结构相变,并且在相变点附近存在较大的体积收缩,相对体积变化率达13%。

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

Data of major andminor elements in magnetite, cassiterite, galena and sphalerite from oredeposits within this ore belt suggest that these ore deposits are of skarn,hydrothermal, porphyry and greisen types related to Yanshanian magmaticactivity and that iron in ores came from regional Permian marine interme-diate-basic volcanic rocks whereas partial lead and zinc from Permian geo-synclinic sediments.

矿带中各矿床的磁铁矿、锡石、方铅矿、闪锌矿的主元素和微量元素数据表明,这些矿床是属与燕山期岩浆活动有关的矽卡岩型、热液型、斑岩型和云英岩型矿床;其成矿金属组分中的铁来源于区域晚古生代海相中-基性火山岩,部分铅锌来源于区域二叠纪地槽沉积物。

China is rich of zinc resource, most of which exist in forms of sphalerite of high iron.

我国锌资源储量丰富,其中有很大一部分以高铁闪锌矿的形式存在。

In this deposit, ore bodies exist in the stratoid form and are c ontrolled by thrust faults. The host rocks are limestone in Bolila Formation of Late Triassic Jiezha Group and in Gadikao Formation of Early-Middle Permian Kaix i nling Group, with strong dolomitization and weak silicification. Minerals are ra ther simple and consist of sphalerite, galena, pyrite, calcite, dolomite and barite. The important ore textures are colloforms such as framboid and crust and xenom orphic grains, and the ore structures are in disseminated, brecciated, veinlike and lumpy forms.

东莫扎抓铅锌矿床矿体呈似层状展布,产状严格受到矿区逆冲断层的控制,赋矿围岩为上三叠统结扎群波里拉组灰岩和下-中二叠统开心岭群尕迪考组灰岩,发育强白云石化和弱硅化,矿物组合简单,主要为闪锌矿+方铅矿+黄铁矿+白云石+方解石+重晶石,矿石结构以皮壳状、草莓状等胶状结构和他形粒状结构为主,矿石构造为浸染状、角砾状、团块状和脉状。

By the studies on typomorphism genesis of mineral paragenesis,composition,morphology and physical properties of the sphalerite,this paper deals with metallogenic source,ore-forming temperature and genetic types of Longjingjie lead-zinc deposit in Taijiang.

通过对闪锌矿的矿物共生组合,成分、形态及物理性质标型特征的研究,讨论了台江龙井街铅锌矿的成矿物质来源、成矿温度及成因类型。

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