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Our experienced high-pressure boiler tubes LU Hong experts believe that in 2010 the international iron ore price agreement will become a reality, but India's exports of iron ore products to its increase in duty bound to curb its exports, which will also lead to international iron ore spot market prices.

我们鲁宏的资深高压锅炉管专家认为,2010年国际铁矿石协议价格上涨将成为事实,而且印度对其出口的铁矿产品加税后,必然抑制其出口,这也将导致国际铁矿石现货市场价格高涨。

The basic principles of the topographic simulation by binary interpolation formula and the ore body bottom and ore body thickness simulation by trend equation were analyzed, and the random formation of schematic section view of ore body was illustrated.

论述了二元插值公式对地形进行模拟、势方程对矿体底板和矿体厚度进行模拟的基本原理,并结合实例对矿体示意剖面的随机生成进行了说明。

Following were the main substances of this research: Rules of import-iron oresagglomeration, import-iron ores include Brazil CVRD iron ore、Indias high qualitymine、Brazil iron fine powder、Irani iron fine powder and Mauritania fine powder.Rules of rich iron ores of Tiangang agglomeration, it includes Laiyuan iron ore andQian'an iron ore.

本文主要研究内容包括:进口富矿粉的烧结成矿规律,进口粉主要包括巴西CVRD 粉、印度高品位粉、巴西铁精粉、伊朗粉和毛里塔尼亚粉;地方精粉主要包括涞源精粉和迁安精粉;在上述研究的基础上,进行合理烧结配矿的研究,从而得出合理的配矿方案和工艺参数。

To Dabaoshan copper ore, at slurry concentration of 10%, lixivium pH of 2. 0, with the domesticated bacterial, copper extraction could reach 27. 84% after 25 days leaching in sample 1〓, in which low grade copper sulfide ore is the main component; in sample 2〓, hypo-sulfide ore is the main component, copper extraction could reach 77. 78% after 10 days leaching.

大宝山铜矿石细菌浸出工艺条件试验研究表明,对于以低品位硫化矿为主的1〓矿,当矿浆浓度为10%、浸出液pH2.0,采用驯化的菌种浸出25天,Cu浸出率可达27.84%;在相同浸出条件下,对于以次生硫化矿为主的2〓矿,浸出10天,Cu浸出率可达77.78%。

The ore is characterized by veinlet structure, net-veined structure and comb structure, and the gradual outward transformation of ore structure from veined via net-veined and veinlet-disseminated to disseminated is common. These characteristics in ore fabrics and the occurrence of cryptoexplosive breccia are strong evidences that Songxi Ag-Sb deposit is a hydrothermal deposit.

矿体中发育大量的脉状、细脉状、网脉状和梳状等充填交代构造,由矿体向围岩常可见脉状→网脉状→细脉浸染状→蚀变围岩的渐变过渡现象,这些构造特征以及热液破碎角砾岩的出现,为嵩溪银锑矿床的浅成热液成因提供了有力证据。

A study of regional geological setting and ore-control factors for the Xiasai Ag-Pb-Zn deposit indicates that NW-trending structures act as conduits for ore fluids and orebodies are controlled by a NNw-trending fault system, while ore shoot s are confined equidistantly to secondary structures associated with the NNW-trending fault system.

研究结果表明,富矿体在NNW向断裂中按一定间距连续出现,并在NNW向断裂伴生的次级构造中集中产出。

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。

Based on the pressure curve experiment, the physical characteristic of ore-bearing rocks of the Luoba lead-zinc deposit in the Qinling Xicheng deposit field shows small porosity, low permeability and bad link ostiole in the ore-bearing rocks series. The feature indicates that the physical characteristic of ore bearing is unfavorable for forming the Luoba lead-zinc deposit.

采用压汞分析技术对秦岭多金属成矿带西成矿田洛坝铅锌矿床含矿层各岩系的物性特征进行了研究,结果表明含矿层各岩系物性特征具有孔隙度小、渗透率低、孔喉连通性差的特点,这一特征对洛坝大型矿床的形成是极为不利的。

Based on the Re-Os isochron method of molybdenites, this paper measured directly the ore-forming age from skarn ore in the Huangshaping deposit, and got a Re-Os age of (153.8±4.8)Ma, which is in accordance with the previous K-Ar age of 153~157 Ma obtained from phlogopite in the ore-bearing skarn of the deposit.

文章采用高精度的辉钼矿Re-Os等时线定年法,直接测得硅卡岩型矿体的矿化年龄为(153.8±4.8)Ma,与前人获得的含矿硅卡岩中金云母的K-Ar年龄(153~157Ma)一致。

In this paper, the petrology, mineralogy and geochemistry of basic-ultrabasic volcanic rock, granite and skarn related to the Sn-Cu skarn-type ore and the vein-type ore in Laochang ore field have been researched systematically, some conclusions are summarized as follows:In Gejiu tin-polymetallic district, the middle Triassic volcanic rocks belonging to calc-alkaline basalt-tholeiite serie, mainly consist of pyroxene, hornblende, feldspar, chlorite and phlogopite; All the granites are peraluminous granites related to the Yanshanian collision-orogeny. Laoka granite closely related to the tin-polymetallic deposits emplaced in the post- orogenic.The metal elements show obviously vertical zones with the variety of skarn types in dimensional extension; The occurrence of garnet skarn and diopside skarn alternately developed in the horizontal zones of the contact between granite and carbonatite are mainly related to two factors: one factor is the infiltration metasomatism of post-magmatic hydrothermal solution, the another is the metrical strata of marble and calcic-dolomite developed in country rocks.

本文重点以老厂矿田中的接触带锡铜矿床和脉状矿床为研究对象,采用化学分析、ICP-MS、X射线粉晶衍射分析、电子探针等测试手段,对本区与成矿相关的基性-超基性火山岩、花岗岩、夕卡岩、电气石-石榴石等进行了系统的地质地球化学研究,研究表明:个旧矿区中三叠纪个旧组地层中的火山岩为钙碱性玄武岩-拉斑玄武岩系列,岩石为辉石-角闪石-长石-绿泥石-金云母组合;本区的花岗岩为过铝质花岗岩,主要与燕山期碰撞造山作用有关,锡多金属成矿与形成时代最晚、分异较好的花岗岩关系密切;本区夕卡岩中的有用共生组份随着夕卡岩类型及其矿物组合的不同具有明显的分带性。

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