辽宁猫岭金矿床地质特征及成因探讨

本文将猫岭金矿床划分为沉积变质、变质热液和交代重熔岩浆热液三个成矿期。由硫、氢、氧同位素,稀土元素特征及包裹体成分研究结果表明变质热液期为主成矿期,主要成矿物质来自围岩,矿床属变质热液成因。     

陕西太白双王金矿八号矿体品位指标的优化

加强低品位金矿床勘查与开发的技术经济合理性研究,已被提到议事日程上来了。合理品位指标的制定则是低品位金矿床勘查与开发技术经济合理性研究中一项十分重要的课题。通过低品位金矿床合理品位指标的研究,不仅可以重新认识和评价我国的黄金矿产资源,而且也是国家最大限度回收和利用黄金矿产资源的战略性措施。陕西省太白县双王金矿为一大型低品位含金角砾岩型金矿,已圈出大小矿体24个,其中八号矿体规模最大。为了满足国家对黄金生产的急需,陕西黄金公司于1986年下达了陕西省太白县太白金矿(双王金矿)八号     

赣东北虎家尖银（金）矿床地质特征及成因探讨

赣东北家家尖矿床系以银为主，伴生金，铅，锌，镉等有益元素的可综合利用的矿床。矿床受中元古界双桥山群中的北东向断裂破碎带控制，其成因为变质热液＋岩浆热液迭加型银（金）矿床。     

Metallogenic mechanisms of super-large Cu and Au deposits in the Dexing region and simulating experiments

Based on the results of previous studies and under the direction of the theory of “ore deposit genesis”, the authors made use of high temperature and high pressure experimental facilities and conditions at the Tectono-geochemistry Research Room under the State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, and put the focus on the multi-source of tectonically controlling ore-forming materials, the characteristics of multi-stage and multi-episode hydrothermal activities and mineralization and the characteristics of multi-genesis and multi-ore deposition so as to shed light on the metallogenic mechanisms of super-large Cu and Au deposits. In addition simulating experiments were made on multi-stage and multi-episode tectonic activities and rock and ore deformation, multi-stage and multi-episode tectonic activities and mobilization and migration of ore-forming materials, and multi-stage and multi-episode tectonic activities and superimposition and enrichment of ore-forming materials. The experimental results showed that under the action of multi-stage and multi-episode tectonic stress the deformation and fragmentation of not only rocks and ores have been intensified, and but also the ore-forming materials originally disbursed in the rocks and ores have been mobilized and migrated and superimposed and enriched. The experimental results also provided the scientific experimental data and grounds for deep-going research on the rules of metallogenesis and geneses of super-large ore deposits in the Dexing region, Jiangxi Province.     

Discrimination Study on Fluid—Rock Interaction Between Metallogenic and Non—Metallogenic Sections in a Shear Zone

Discriminations in a local chemical,fluidal,mechanical and thermal processes in a shear zone will lead to metallogenic differentiation in a local section.This paper,based on the general geological setting of the Shibangou gold deposit in Xixia,Henan,deals with petrological and petrochemical samples of altered rocks in the metallogenic section and of mylonites in the non-metallogenic section of a selected shear zone.The discriminations in fluid-rock interaction and petrological mass balance between altered rocks near the orebody and mylonites in the shear zone are discussed as well.The results show that the petrological volume of altered rocks in the metallogenic section of the shear zone is almost always dilatant and the mylonite volume in the non-metallogenic section is almost always lost.Major elements in altered rocks from the metallogenic section and in mylonites from the non-metallogenic section always show a tendency of being enriched and depleted,respectively.Fluid-rock ratios in the mylonites(Nu=93.68-468.40)are larger than those of the altered rocks(NC(Ⅳ）^s=36.11-216.67).The gain and loss of major and trace elements from the altered rocks and mylonites in the shear zone are a composite process to be imported and exported by percolating fluids as well as of the loss and dilatancy of rock volume.     

李坝金矿床金的赋存状态与选矿工艺学

李坝大型金矿床是产于西秦岭上古生代沉积岩系中类卡林型金矿床典型代表。通过显微镜及选矿实验查定了李坝金矿床金的赋存状态，矿床金矿物呈微细粒多种独立矿物出现，金的赋存形式多样，显示多期多阶段成矿特点，成为划分类卡林型金矿的重要参考。矿石工艺学的研究对工业选矿有指导意义。     

四川木里梭罗沟金矿床特征

四川木里梭罗沟金矿床位于甘孜—理塘构造成矿带的南段、唐央复式背斜南东倾伏端(或唐央穹窿南缘),目前已探明储量属大型岩金矿床。矿体产于上三叠统曲嘎寺组蚀变基性火山岩中,受近东西向断裂控制。矿床具多期成矿特点,属构造蚀变岩型—中低温热液型金矿床。     

甘肃礼县中川地区金矿流体的来源与成因

甘肃省礼县中川地区属于礼（县）岷（县）金矿带的东段,其成矿作用与中川花岗杂岩体有密切的关系。此次研究在已知金矿体上采集标本,碎样后挑选石英晶体,运用英国Micromass公司生产的MM5400质谱计,在1 600℃条件下,让石英释放稀有气体,测量其中的⁴He、²⁰Ne、⁴⁰Ar等稀有气体,通过稀有气体的示踪作用,研究成矿流体的来源。测试结果表明：礼县中川地区金矿的成矿流体中的⁴He和⁴⁰Ar来源于中川花岗杂岩体;Ar同位素比值符合地壳流体特征;在³He/⁴He-⁴He/²⁰Ne体系图上,7个样品中,有4个点位于100%地壳流体来源线上,3个点位于5%上地幔与30%上地幔流体之间,说明成矿热流成分主要是地壳流体,含有10%左右的上地幔热流,即礼县中川地区金矿成矿流体具有混合热液特征。     

秦岭煎茶岭金矿床含金富砷黄铁矿增生环带研究

在秦岭剪茶岭金矿床中发现了含金富砷黄铁矿增生环带。其产状,结构构造和成分特征共同显示了,金成矿主期金与砷有密切的地球化学相关性,在富砷增生环带发育时,金与砷共沉淀并可能在其中发育了不可见金。这种环带包含有重要的成矿作用信息,至少在矿区范围内可用于判别是否有主期矿化发育。     

CO_2-H_2O流体不混溶对Au溶解度的影响——以贵州省贞丰县水银洞金矿床为例

运用热力学原理和方法,研究了CO2-H2O流体不混溶作用对Au的溶解度的影响。结果表明,贵州水银洞金矿床的成矿流体是一种富含挥发分（fCO2=70.79MPa）、酸性（pH=3.71）、还原性（fO2=0.50×10-36MPa）、中温（267℃）、具有超压（180MPa）性质的含Au（a∑Au=3.744×10-8mol/L）流体。当超压流体的封闭层——炭质页岩因断裂作用而被破坏时,热液体系的压力发生骤降（28.50～35.30MPa）,CO2-H2O流体发生不混溶作用,并有大量CO2溢出。CO2的流失可使成矿溶液的CO2逸度和O2逸度降低（fCO2=0.80MPa、fO2=2.512×10-42MPa）,酸碱度升高（pH=4.32）,同时伴随温度的下降（224℃）,成矿热液中Au溶解度的降低（a∑Au=3.790×10-9mol/L）,从而快速沉淀下来成矿。