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As a powerful company in the field of mineral resources, Shanghai Runxi Commercial Enterprise Co., Ltd. boasts quality nickel ore, iron ore, etc., involves and invests in such projects as power plant and ferronickel factory in Southeast Asia.

上海润希商贸有限公司是一家实力雄厚的矿产资源公司,在亚洲拥有高品质的镍矿、铁矿矿山,并在东南亚地区参与投资建设电厂、镍铁工厂等项目。

The company produces the product widely uses in classifying the titanium, the gold, the silver, the copper, the iron, the tungsten, the lead, the cobalt, mo, zinc, tin, molybdenum, nickel, stibium, tantalum, niobium, manganese ore, fluorspar, coal, monacite, rutile, other rare metals and precious metal ore and so on.

公司生产的产品广泛用于选别钛,金,银,铜,铁,钨,铅,钴,镆,锌,锡,钼,镍,锑,钽,铌,锰矿石,萤石,煤,独居石,金红石,其它稀有金属和贵金属矿等。

In the wet-process phosphoric acid production from the Hubei phosphate ore, one of the bothersome problems is that potassium fluosilicate and sodium fluosilicate scales are liable to form on the filtration system owing to its high potassium and sodium content, which greatly restrains the application of Hubei phosphate ore.

本文首先采用人工冷却系统模拟湿法磷酸生产的真空过滤系统冷却过程,研究垢物的析出规律,实验结果得知:垢物的主要成分为氟硅酸钠和氟硅酸钾,氟硅酸钠首先析出,结构致密,其次是氟硅酸钾,最后是二水硫酸钙,氟硅酸钠对氟硅酸钾有很强的结晶诱导作用;然后在三种生产中常用的不同的材质钼二钛、聚氯乙烯和聚四氟乙烯表面进行结垢试验,发现聚四氟乙烯表面最不易结垢,而在钼二钛表面最易结垢。

According to craft mineralogical research result, use raw ore to wait for sulfide via floatation eliminate realgar, gamboge first, soak of the cyaniding after floatation concentrate pretreatment, the plan of direct cyaniding soak undertakes floatation gangue experiment, total soak rate of gold is achieved 88.52%, relatively raw ore is direct soak of complete mud cyaniding increases 25.02 percent.

根据工艺矿物学探究结果,采用原矿先经浮选除去雄黄、雌黄等硫化物,浮选精矿预处理后氰化浸出,浮选尾矿直接氰化浸出的方案进行试验,金的总浸出率达到88.52%,较原矿直接全泥氰化浸出提高25.02个百分点。

The studies on ore-forming geochronology and ore fluid are conducted deeply in this paper.

本文对甘肃北山地区肃北县南金山金矿床的成矿年代学和成矿流体进行了系统研究。40Ar-39Ar同位素测年结果表明,南金山金矿石中绢云母的40Ar/39Ar坪年龄为242.8±0.8Ma,相当于印支早期,略晚于南金山金矿床附近闪长岩中黑云母的40Ar/39Ar坪年龄(244.2±0.3Ma),这表明印支早期闪长岩对南金山金矿床的形成起着重要的控制作用。

Studies on petrochemistry , geochronology of diagenetic and ore formation, mineralization and ore assessment of Baogutu porphyry copper deposit were done.

本论文分别从矿床地质、岩石化学、成岩成矿年代、成矿作用等方面对包古图斑岩铜矿床做了系统研究。

The results showed that Weipa ore is gibbsite and its leaching efficiency is high when digested at higher than 200 ℃,so applicable to sweetening ore in digestion process,under conditions that the sweetening process is controlled in the range of 195~200 ℃ for 15~20 min and the dosage of Weipa .

对澳大利亚韦帕矿的溶出性能及以韦帕矿为后加矿的增溶溶出技术进行了实验研究。考察了增溶温度,增溶时间,后加矿加入量对溶出效果的影响,同时对后加矿增溶溶出的矿浆性能进行了对比性研究。结果表明:韦帕矿为三水铝石矿,在200℃以上溶出时,浸出率较高,适宜作为增溶溶出过程的后加矿。以韦帕矿为后加矿,其适宜的增溶溶出条件为:增溶温度195~200℃,增溶时间15~20 min,后加矿的质量分数为15%~20%。后加矿增溶溶出矿浆具有优良的沉降压缩性能

To probe the ore-controlling factor s and origin of Jinshan Gold Deposit,on the basis of studying the geological background of minerallization,by adopting the comprehensive geological and geochemical method,this paper analyzes the strata,structure,magmatic rock,ore-body character,stable isotop,temperature,pressure and flouid of minerallization and trace elements in the mining area.

为了研究金山金矿的控矿因素及矿床成因,在研究成矿地质背景的基础上,结合野外地质及前人研究成果,采用地质、地球化学综合分析的方法,对矿区内地层、构造、岩浆岩、矿体特征、稳定同位素、成矿温度压力、成矿流体及微量元素特征进行了剖析。

To probe the ore-controlling factors and origin of Jinshan Gold Deposit,on the basis of studying the geological background of minerallization,by adopting the comprehensive geological and geochemical method,this paper analyzes the strata,structure,magmatic rock,ore-body character,stable isotop,temperature,pressure and flouid of minerallization and trace elements in the mining area.

为了研究金山金矿的控矿因素及矿床成因,在研究成矿地质背景的基础上,结合野外地质及前人研究成果,采用地质、地球化学综合分析的方法,对矿区内地层、构造、岩浆岩、矿体特征、稳定同位素、成矿温度压力、成矿流体及微量元素特征进行了剖析。

Mine is too ancient geological ore mixed granite and granite porphyry, ores major components of SiO2, accounting for 76.54%, Al2O312.56%, Qianhui, the fine-grained gray granite block change crystal structure, long-ramp of 27 -- 36 percent, longer-35-42 percent, 20-29 percent quartz, rock weighing 2.6 T/m3, hardness of 5.9-6.3 degrees, the porosity of 0.62-1.03 percent, compressive 1670-1931 kg/cm2, bending 141-167 kg / cm2, ore reserves 2000 investigation Grade D geological reserves 10.02 million cubic meters, designed for the use of reserves of 7.99 million cubic meters; mining area of 0.4 cubic kilometres, the highest elevation of 151 meters, the minimum 56 meters, hilly slope, with perennial Shuixi, More sparse vegetation.

矿山地质矿体属太古代混合花岗岩及花岗斑岩,矿石主要成分SiO2,占76.54%,Al2O312.56%,浅灰,灰白色的细粒花岗变晶块状构造,斜长石含量27-36%,更长石35-42%,石英20-29%,岩石体重2.6T/m3,硬度5.9-6.3度,孔隙度0.62-1.03%,抗压1670-1931kg/cm2,抗折141-167kg/cm2,矿石储量2000勘测D级地质储量1002万立方米,设计利用储量为799万立方米;矿区面积0.4立方千米,最高海拔为151米,最低56米,丘陵缓坡,无常年水溪,植被较稀疏。

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