低场理论及有利找矿标志

找铀矿要到放射性高异场中去找,这似乎已成为一种习惯,因而也影响找矿效果．实践表明,约有80％的矿是位于低异常场及与之相邻的离异常场附近,特别是面积为几十平方公里的小高异常场中通过对国内外上千个矿田、矿床和矿点的统计研究,提出在自然界中存在着呈“萝卜型”分布的异常（矿床或矿体）为核心的低场理论、探讨了低异场产生的机制,总结了低场中的10种有利找矿标志．对两个地区今后的勘查进行了有益的讨论     

汕头港及其邻近水域潮间带海产动物体内重金属污染的调查

调查了汕头港及邻近水域潮间带常见海产动物体内的重金属含量。结果表明，翡翠贻贝(Perna viridis)体内的Ni、鳞笠藤壶(Tetraclita squamosa squamosa)体内的Cr和Zn、近江牡蛎(Crassostrea rivularis Gould)体内的Cu和Zn含量高于海洋生物污染评价标准。近江牡蛎的Cu污染因子质量分指数最高达6．01。可食性贝类中疣荔枝螺(Thais clavigera)体内的Cd、Zn，翡翠贻贝体内的Cd、Ni和Pb，小荚蛏(Siliqua minima)体内的Cd、Ni，近江牡蛎体内的Cd、Cu、Ni和Zn的含量高于人体食用限量标准。其中近江牡蛎体内的Zn含量最高，为限量标准的23．5倍。港内比港外污染严重，远离港口站位的生物体内重金属含量仍有超标现象，表明汕头港及其邻近水域的重金属污染严重。     

Copper and zinc isotope variations in ferromanganese crusts and their isotopic fractionation mechanism

Ferromanganese(Fe-Mn) crusts are potential archives of the Cu and Zn isotope compositions of seawater through time. In this study, the Cu and Zn isotopes of the top surface of 28 Fe-Mn crusts and 2 Fe-Mn nodules were analysed by MC-ICP-MS using combined sample-standard bracketing for mass bias correction. The Zn isotope compositions of the top surface of Fe-Mn crusts are in the range of 0.71‰ to 1.08‰, with a mean δ~(66) Zn value of 0.94‰±0.21‰(2 SD, n=28). The δ~(65) Cu values of the top surface of Fe-Mn crusts range from 0.33‰ to0.73‰, with a mean value of 0.58‰±0.20‰(2 SD, n=28). The Cu isotope compositions of Fe-Mn crusts are isotopically lighter than that of dissolved Cu in deep seawater(0.58‰ vs. 0.9‰). In contrast, the δ~(66) Zn values of Fe-Mn crusts appear to be isotopically heavy compared to deep seawater(0.94‰±0.21‰ vs. 0.51‰±0.14‰). The isotope fractionation between Fe-Mn crusts and seawater is attributed to equilibrium partitioning between the sorption to crusts and the organic-ligand-bound Cu and Zn in seawater. The Cu and Zn isotopes in the top surface of Fe-Mn crusts are not a direct reflection of the Cu and Zn isotopes, but a function of Cu and Zn isotopes in modern seawater. This study proposes that Fe-Mn crusts have the potential to be archives for paleoceanography through Cu and Zn isotope analysis.     

A study on zinc speciation of Tungabhadra River sediments,Kurnool, south India: A tool in metal pollution monitoring

The Tungabhadra River is one of the sacred rivers in south India. Industrial and mining operations on its banks generate enormous amounts of effluent that have led to substantial metal and nutrient contamination of the aquatic system. In the present investigation an attempt has been made to assess variation in the physico-chemical characteristics and speciation of zinc in the water and sediment of the Tungabhadra River. Most of the metal ions in the collected samples were in high concentrations compared to the applicable standards. The Individual Contamination Factor (ICF) of Zn was found to be more at Site-B compared to sites A and C. Zinc-bearing particles were characterized by the different morphologies measuring from large colloidal to small particles which were associated with biological structures or may be present in amorphous nature which were observed by Transition electron microscopy (TEM) with X-EDS (Energy dispersive spectrometry). In conclusion, the level of Zn contamination in the Tungabhadra River is increasing at an alarming rate due to industrial activities.     

含铁闪锌矿热力学性质的推导

热容是矿物热力学性质的基础,通过热容测定,可以推导出矿物的其他热力学性质,本文在对３个含铁闪锌矿样品的热容进行实验测定的基础上,推导出它们的热力学性质,本文的研究结果为系统地研究闪锌矿及其成矿物理化学条件参考数据。     

青海锡铁山铅锌矿床喷流沉积后的构造再造过程

本文提出锡铁山矿区早期属伸展构造体制,形成加里东期变质核杂岩;晚期属收缩构造体制,形成海西期褶皱冲断岩片。认为基底剥离断层(F1)与上剥离断层(F2)所夹绿色变质岩系(O3tna -b)属绿片岩相顺层正滑韧性剪切带,带内基性 -中酸性火山岩所夹灰岩层经变形分解作用形成大理岩构造透镜体群,并在递进变形过程中经水力压裂作用在其中形成系列雁行排布的Y或R型张裂构造,而原先赋存于海相火山岩中由喷流沉积作用形成的层控铅锌矿体则完全从高应变带内迁出,继而沉淀于低应变的透镜化大理岩中及其附近的新生容矿空间中。重点阐述了大理岩透镜体的几何特征,并依此提出预测隐伏铅锌矿体的地质依据     

高精度预测模型及其构建方法——以脉状金矿为例

采用“场理论—场结构—场分析—场模拟”方法构建了具有时空结构框架,能反映局部异常精细结构特征,可对多元预测信息进行有效提取和集约 化分析的高精度预测找矿模型。该模型是对致矿异 常结构、矿化结构和信息结构的耦合分析与关键预测信息提取及优化相匹配和深化后的最佳 表达方式。其技术关键是预测对象的地质、地球物理、地球化学异常场和成矿场的精细结构 分析以及矿体空间定位产状模式的建立。     

Seasonal Cycles of Dissolved Cd, Mn and Zn in River Water Caused by Variations in pH Induced by Biological Activity

pH, dissolved oxygen, Zn, Cd and Mnwere measured once a month for 2.5 years in the LotRiver, France. The pH is controlled by biologicalactivity (photosynthesis and respiration). Dissolvedoxygen variations are due to a combination ofbiological activity and of the temperature dependenceof the oxygen solubility. pH is the master variablefor concentrations of aqueous Zn, Cd and Mn, thelowest concentrations being associated with thehighest pH values, which occur during the summer. pH-related processes rather than redox phenomenaexplain variations in dissolved Mn. Variations indissolved Zn and Cd are also controlled bypH-dependent reactions (possibly related to thedissolutive behavior of solid Mn).     

中朝古元古代层控铅锌矿床类型及其比较

中朝古元古代层控铅锌矿床属海底喷气沉积铅锌矿床。以地层对比与含矿层位为基础,以铅、硫同位素为重要信息,结合后期地质事件对矿床的影响与矿床主要成矿阶段的不同,将这类矿床划分４个类型：受变质沉积层控铅锌矿床（大栗子式）、受改造沉积层控铅锌矿床（张家堡子式）、变质热液改造型层控铅锌矿床（检德式）和岩浆热液叠生型层控铅锌矿床（青城子式）。从成矿氛围、矿体、伴生矿与共生矿、矿物组合、结构与构造、蚀变、地球化学特征、稳定同位素、成矿物理化学条件、远景评价１０个方面比较,发现它们每一项都是既有相同点,又有相异点,证明了大类型的相同和小类型的差别。     

重金属对扁额细首纽虫金属硫蛋白的影响

生物体内金属硫蛋白含量变化,可作为环境中重金属污染的生物标志物.通过暴露实验研究了扁额细首纽虫Cephalothrix simula暴露在不同浓度的铜,锌和镉溶液96 h,其体内金属硫蛋白含量的变化规律.结果表明3种重金属离子的胁迫作用均导致金属硫蛋白含量增加,在实验初期(6～24 h),金属硫蛋白含量达到高峰;金属硫蛋白含量与暴露溶液金属浓度具有明显的剂量～效应关系,金属离子浓度越高,金属硫蛋白含量越高;锌离子诱导金属硫蛋白合成的作用大于铜、镉离子.