滑脱构造与黔西南地区金矿浅析

己被国内地质学界广为重视的黔西南地区微粒侵染型金矿,矿床的分布和富集严格受低角度断层控制。笔者从地壳内多层滑脱的观点出发,结合研究区的典型矿床实例,将该区域内不同矿区,不同控矿特征的金矿床,纳入地壳浅部多层滑脱构连的统一模式中进行讨论,并据此对深部原生矿产富集的有利部位进行了预测分析。本文的目的在于,通过黔西南地区地壳浅层构造的理论分析,为该区的金矿普查与勘探提供一条新的思路。     

四川拉拉地区天生坝铁矿中铜矿化的发现及地质意义*

通过野外地质调查,在四川拉拉地区天生坝铁矿露天采场发现铜矿化。铜矿化主要表现为黄铜矿-黄铁矿细脉沿围岩裂隙分布和黄铜矿-黄铁矿星点状分布于角砾之间,脉状矿石铜品位0.05%~0.44%,平均0.28%;角砾状矿石铜品位1.54%~1.60%,平均1.57%。黄铜矿交代磁铁矿和黄铁矿,黄铁矿呈交代残余包裹于黄铜矿中。矿石具有较低的初始~(143)Nd/~(144)Nd比值(0.510 626~0.510 811)、负ε_(Nd)(t)值(-2.89~-6.51)和均一的硫同位素(δ~(34)S_(CDT)∶1.4‰~2.0‰)。总之,天生坝铜矿化特征和地球化学特征,均与落凼铜矿特征一致,具有典型的铁氧化铜金矿床特征。天生坝铁矿铜矿化的发现,表明拉拉地区F1断层以南具有较大的找矿潜力,天生坝铁矿深部的河口群变质火山岩值得进一步工作。     

潘洛铁矿滑坡特征分析及防治

分析了潘洛铁矿露天矿滑坡灾害发生发展的特征,得出该滑坡是一个动态的、多层次的复合型滑坡;找出了影响该边坡稳定的主要因素是大气降雨和采矿切割坡脚;根据这些影响因素和滑坡发展变化规律,提出了科学合理的滑坡治理方案,即动态的综合治理方案.经现场实施后,通过滑坡监测数据表明,该滑坡得到了彻底根治.     

Hydrometallurgical application for treating a Nigerian chalcopyrite ore in chloride medium: Part I. Dissolution kinetics assessment

The dissolution kinetics of a Nigerian chalcopyrite ore in hydrochloric acid was studied in this article. Acid concentration, reaction temperature, and ore particle size were chosen as experimental parameters. The chemical and morphological studies of the ore before and after leaching at optimal conditions were carried out by X-ray diffraction (XRD) and scanning electron microscopy (SEM). It is revealed that increasing the acid concentration and system temperature and decreasing the ore particle size greatly enhances the dissolution rate. The dissolution kinetics was found to follow the shrinking core model for the diffusion control mechanism where the activation energy (E_a) of 32.92 kJ·mol?1 was obtained for the process and supported by morphological changes at a higher dissolution of 91.33%.     

铁矿石粉矿成分对烧结强度的影响

在铁矿石烧结过程中,熔体性质决定了烧结矿粘结相的结构.采用小型试验来考察铁矿石粉矿的化学成分(SiO2,Al2O3,MgO和碱度)对烧结强度的影响.并通过化学成分对熔体的黏度和表面张力的影响来对烧结强度的变化加以解释.试验结果表明,随着粉矿中配加CaO与矿石的质量比的变化(0.08~0.15),在CaO与矿石质量比为0.12时获得最大烧结强度;而碱度R=2时获得最大的烧结强度;随着MgO含量的增加其烧结强度逐渐降低;而烧结原料中Al2O3质量分数不宜超过2.5%.     

西藏谢通门县雄村铜(金)矿矿石物质成分研究及其意义

西藏谢通门县雄村铜(金)矿是新发现的超大型细脉浸染型铜(金)矿.通过详细的岩石学、矿石学研究,表明矿石类型主要分为氧化矿石、次生硫化物矿石和细脉浸染状硫化物矿石三大类型.矿石主要为细脉浸染状.主要金属矿物为黄铜矿、黄铁矿、磁铁矿、磁黄铁矿,其次是辉铜矿等.主要非金属矿物为石英,约占矿物总量的60%～70%;其次是红柱石、钾长石、斜长石、黑云母、白云母、绢云母、绿帘石、石榴子石等.矿石主成矿元素以Cu为主,伴生有用组分为Au,Ag,Zn和Pb等.     

铁尾矿试制微晶玻璃的研究

研究了以选铁尾矿为主要原料，采用淬粒法工艺制作微晶玻璃的配方、熔化温度、晶化温度、保温时间等工艺参数，并对样品的性能进行了检测，分析了影响样品质量的主要因素。     

柴西北缘花土沟地区新近系油砂山组沉积特征及铀源分析

柴北缘花土沟地区新近系油砂山组含铀岩系为绿灰色碎屑岩沉积建造。区域内主要发育扇三角洲、滨浅湖相。含铀岩系受滨浅湖相沉积体系控制。研究区内铀源具有多源性特点,基底和盖层铀丰度较高。通过野外调查实测剖面和编录铀矿调查钻孔发现油砂山组具有泥-砂-泥结构特征,砂层厚度适宜,倾角较缓,属于宽缓的山前斜坡带,有利于含矿砂体及富氧流体进入层间,形成层间氧化带及铀的富集。     

固相反应合成稀土钙钛矿氧化物的研究

采用固相反应方法合成了稀土钙钛矿型氧化物-SmCoO3，并利用XRD和Raman谱对其结构进行了测试，确定了合成单相SmCoO3的条件及反应时间对合成产物的影响。     

赞比亚卢安西亚矿区复杂铜矿孔雀石的机械活化及浸出研究

Mechanical activation(MA) of malachite was carried out by dry planetary grinding(DPG) and wet Isa grinding(WIG) methods. When the rotational speed was increased to 400 r/min in DPG, the specific surface area of malachite reached the maximum and the particle size reached the minimum of 0.7–100 μm. Agglomeration occurred between mineral particles when the rotational speed was increased to 580 r/min in DPG.However, no agglomeration was observed among particles with sizes 0.4–3 μm in WIG. X-ray diffraction analysis showed that, at a 580 r/min rotational speed in DPG, the amorphization degree of malachite was 53.12%, whereas that in WIG was 71.40%, indicating that MA led to amorphization and distortion of crystal structures. In addition, in the Fourier transform infrared(FT-IR) spectra of activated malachite, the bands associated with –OH, CO_3^2-and metal lattice vibrations of Cu–O and Cu–OH were weakened, and a new H–O–H bending mode and peaks of gaseous CO_2 appeared, indicating that MA decreased the band energy, enhanced dihydroxylation, and increased the chemical reactivity of the malachite.Furthermore, the leaching behavior of copper ore was greatly improved by MA.