Comparison of metallogenesis and resource potential on the eastern margin of the Jiangnan Upheaval between south Anhui (Wannan) and northeast Jiangxi (Gandongbei) provinces

The southern and northern parts of the eastern margin of the Jiangnan Upheaval, located in the northeast of Jiangxi Province (Gandongbei) and the south of Anhui Province (Wannan) share many similar characteristics of basement composition and structural evolution. However, the two areas have very different metal endowments and ranges of deposit types. The aim of this paper is to compare the metallogenic conditions of the two areas in order to analyze the reasons for these differences and to estimate the preliminary resource potential of the studied areas. It is concluded that difference of the crust-mantle interactions, especially the Yanshanian magmatism in the two areas, is the main reason resulting in difference in the ore-forming processes between Wannan and Gandongbei. The resource potential of Gandongbei is significantly greater than that of Wannan.     

白银厂矿田同位素特征及其流体成矿作用研究

白银厂矿田多金属硫化物矿床的石英包裹体水的δD水为-71‰～95‰，δ^18O水为-0．09‰～ 8．7‰，显示了岩浆水、大气降水、变质水的混合作用．含矿火山岩总硫δ^34S∑s( 3．68‰)指示硫主要为深部岩浆来源，并经历了陆壳硫的混染，矿石硫主要来源于围岩．含矿流纹岩中的铅为地幔和地壳的混合铅，矿石铅主要来自嗣岩的构造活化铅．这些同位素特征研究表明，白银厂矿田经历了两期成矿作用．早期为岩浆流体与大气降水混合成矿；晚期为构造流体与大气降水混合．对流循环成矿．     

Biomarkers in fluid inclusions of polymetallic deposit of Qixiashan, Nanjing

Conclusions Organic fluid involved in Pb-Zn mineralization in the polymetallic deposit of Qixiashan probably derives from bacteria and algae, and is similar to that of the mature crude oil system. Part of lead and zinc in fluids can be transported by organic complexes, while their precipitation is caused by organic reduction. Biomarkers in ores can indicate the source of organic matter in fluids, but organic matter in inclusions must be studied to ascertain organic metallogenesis because of the EOM difference between ores and inclusions. The host strata of Upper Carboniferous (C2) and Lower Permian (PI) in Qixiashan deposit are both oil-bearing in the region. Identification of organic fluid and its biomarkers in the deposit provides significant information for further studies on the relationship between ore deposits and oil pools in the region.     

Experimental study of gold distribution in the algae-organic matter-fluid system

Conclusion Gold distribution and transformation in algae-organic matter-fluid system is very complicated. Gold is first concentrated in kerogen after algae died. With the increase of dissolved organic matter owing to the increase of temperature and pressure, part of gold simultaneously emigrates from kerogen to DOM. When DOM forms organic fluid and emigrates from the strata, gold is simultaneously carried away by organic fluid in acidic condition, but by water in alkali condition. When the auriferous fluid flows through carbonaceous strata, gold in fluid is unloaded by kerogen. Gold migration in the system, accompanied by the evolution of algae-organic matter-fluid, provides the basic information of biometallogenetic evolution of gold.     

云南迪庆春都斑岩铜矿床S、Pb同位素组成—成矿物质来源的指示

春都铜矿是中甸岛弧带西斑岩带的一个典型矿床,对春都铜矿床矿石矿物开展了S、Pb同位素地球化学研究。矿区硫同位素组成非常稳定,黄铁矿、黄铜矿和方铅矿的~(34)δS值分别为-3.0‰~-0.14‰(平均~(-1).09‰),-6.54‰~-2.11‰(平均-3.44‰),-5.0‰~-3.6‰(平均-4.07‰)且依次降低,表明硫化物沉淀过程中硫同位素分馏基本达到平衡。16件硫化物样品的34δS均值为-2.41‰,表明硫主要为深部岩浆来源。矿石矿物铅同位素~(206)Pb/~(204)Pb,~(207)Pb/~(204)Pb,~(208)Pb/~(204)Pb比值分别为17.863~18.036,15.448~15.614和37.753~38.188,不同样品的铅同位素组成表明铅可能具有多源性,所有样品铅同位素投点均落入造山带区域或上地壳,表明铅具有壳幔混合来源的特征。这种硫铅同位素组成表明岩浆可能起源于俯冲洋壳板片的部分熔融并受到少量地壳物质的混染。     

广西九毛锡矿床的成矿物理化学条件和锡的迁移形式

本文根据九毛锡矿产出的地质地球化学环境,定量计算了成矿作用的物理化学参数。首次提出并讨论了锡矿的中低温成矿作用,从而打破了锡矿元素只在高温条件下才能成矿的传统观念。成矿作用主要在中低温(260～160℃)热液阶段,压力500×10~5～340×10~5pa,氧逸度log fo_2=-29.2～-42.5,硫逸度log fo_2=-7.7～-19.25,pH=6.1～4.5。运用络合物化学原理和方法,定量计算了成矿流体中锡主要呈羟基络合物形式迁移。     

庐枞北部火山-次火山成矿作用过程REE分异特征

文章分析了庐枞北部火山-次火山成矿作用过程中稀土元素的分异特征,将该区火山-次火山气液型矿床的主要矿石矿物的稀土配分模型分为3种类型:平坦型、跳跃型和倾斜型;同时还分析了龙桥铁矿床稀土元素分异的定向性演化特征,即成矿由早阶段到晚阶段,随温度的降低,稀土元素的演化趋势是向Eu负异常增大和轻/重稀土元素比值降低的方向进行,稀土配分曲线由倾斜趋于平缓。