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In addition to Fe+(54Fe+, 56Fe+, 57Fe+), other fragment ions were detected in bacteriogenic pyrites, such as 27 Al+, Si+(28Si+, 29Si+, 30Si+), 40Ca+, Cu+(63Cu+, 65Cu+), Zn+(64Zn+, 66Zn+, 67Zn+, 68Zn+), Ni+(58Ni+, 60Ni+, 62Ni+), and C3H7+.

在杆状菌落成因的黄铁矿中,检测到的组成有 Fe+(54 Fe+、56 Fe+、57 Fe+)、 27 Al+、 Si+(28 Si+、29 Si+、30 Si+)、40 Ca+、 Cu+(63 Cu+、65 Cu+)、 Zn+(64 Zn+、66 Zn+、67 Zn+、68 Zn+)、 Ni+(58 Ni+、60 Ni+、62 Ni+)、 C3H7+。

Six kinds of minerals, such as pyrites, arsenopyrite, sphalerite, galena and cassiterite from various metallogenic stages, ore blocks and ore type s were analyzed by EMPA.

文章总结和划分了矿床的矿石类型、矿化阶段及其在空间上的分布;对不同阶段、不同地段和不同类型的黄铁矿类、毒砂、黄铜矿、闪锌矿、方铅矿和锡石等 6种主要矿石矿物进行了电子探针微区分析。

The mineral mode of Cassiterite, Jamesonite, Marmatite, Arsenopyrite, Pyrite and Magnetic Pyrites are established on the basis of the the grade model of No.100 ore-body. The maps of sections and planes are plotted and the mineral deposit is calculated.

在矿床品位建模的基础上建立了锡石、脆硫铅锑矿、铁闪锌矿、毒砂、黄铁矿和磁黄铁矿等六种矿物的矿物模型,并编制了各种图件和进行了矿物量的计算。

Fluorites formed in uranium mineralization period in the Zoujiashan and Shazhou uranium deposits have ε〓 values from -6.7 to -8.3 and I〓 values from 0.7145 to 0.7204, similar to their host rocks (porphyroblastic lava and sub-granodioritic porphyry) which have ε〓 values from -6.2 to -9.4 and I〓 values from 0.7121~0.7192. On diagram of ε〓- t, the fluorites and host rocks plot in similar area within the evolution field of the basement rocks at Xiangshan. The lead isotopic compositions of pyrites formed in uranium mineralization period plot as a line on diagram of 〓Pb/〓Pb vs.〓Pb/〓Pb. The host rocks plot at the lower value end. Calculation based on the slope of the line and the mineralzation age yields age of 144Ma for the geological body which provided uranium for the mineralization.

邹家山和沙洲铀矿床成矿期萤石的ε〓值(-6.7~-8.3)和I〓值(0.7145~0.7204)与赋矿围岩(碎斑熔岩及次花岗闪长斑岩)的ε〓值(-6.2~-9.4)和I〓值(0.7121~0.7192)相似,在ε〓-t图上,成矿期萤石数据点的投影范围与赋矿围岩的基本吻合,且均落在相山元古宙基底演化域范围内;成矿期黄铁矿的铅同位素组成在〓Pb/〓Pb-〓Pb/〓Pb关系图上呈线性分布,而火山岩的铅同位素组成位于此相关线的低值一端;利用异常铅线的斜率及成矿年龄计算出富铀地质体的形成年龄为144Ma,这与赋矿围岩的成岩年龄(135~140Ma)非常接近。

When the heap of pyrites had been entirely reduced by fire, the result ofthe operation, consisting of sulphate of iron, sulphate of alumina, flint,remains of coal, and cinders was placed in a basinful of water. Theystirred this mixture, let it settle, then decanted it, and obtained a clearliquid containing in solution sulphate of iron and sulphate of alumina, theother matters remaining solid, since they are insoluble.

大堆的黄铁矿石经过加热以后,完全还原了,他们把得到的硫酸铁、硫酸铝、火石、炭渣和灰烬全放在一只盛满了水的盆子里,把这种混合物搅和一阵,接着让它沉淀,然后把水倒出来,得到一种含有硫酸铁溶液和硫酸铝溶液的纯净液体,其他不能溶解的物质,还保持着固体的状态。

In these several years, the company has cooperated with German Lurgi and Nanjing Chermical Industrial Group Design Institute to develop the series of products of waste heat boiler of sulfuric acid made of pyrites. This product and blowing air waste heat boiler are selected as Specially-designated Products. Regarding the cement kiln low temperature waste heat recovery, the company has fully introduced and digested advanced domestic and foreign technologies and has achieved great success. The company has marched into metallurgical industry in 2004, established cooperation with numerous large scale metallurgical institutes and successful developed series of products of waste heat boilers in metallurgical industry, especially sinter cooler low temperature waste gas residual heat power generation boiler. It has successively developed the products such as converter waste heat boiler, electric furnace waste boiler etc.

近几年,公司与德国鲁奇、南化设计院合作研制开发了硫铁矿制酸余热锅炉系列产品,该产品与吹风气余热锅炉被《化工工程建设标准》选为定点产品;在建材行业水泥窑低温余热回收上,充分引进消化国内外先进技术,并取得骄人成绩,2004年进军冶金行业,与国内众多大型冶金院建立了合作,成功开发了冶金行业余热锅炉系列产品,特别是烧结冷却机低温废气余热发电锅炉,又相继开发了转炉余热锅炉、电炉余热锅炉等产品。

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