印尼古邦岛(KUPANG)卡菲默纳努(KEFAMENANU)千岛矿区 锰矿地质特征及成因探讨

印尼千岛锰矿贮存于白垩系上统砂岩、泥岩中,呈层状、似层状产出,具有层控特征,局部遭受断裂构造破坏。通过对矿区成矿地质条件分析,初步认为矿床属于海相碎屑沉积类型锰矿床,具有较好的找矿远景。     

酸溶——催化极谱法测定地质样品中的钨、钼

本文采用混合酸溶解样品,对影响催化体系稳定的酸度、温度和不同反应时间的因素分别进行了对比试验,确定催化体系相对稳定的最佳条件,经过大量样品的分析验证,分析方法可靠。     

商城县汤家坪钼矿地球化学特征及找矿远景

矿区地质、地球化学特征研究入手,总结了综合找矿标志,指出了进一步找矿方向。研究表明该矿床成矿组分单一,异常元素组合主要为Mo、Bi、Ag,次为W、Sn、Zn、Cu、Pb,仅有钼能形成较大规模的异常;矿床元素水平分带序列为(Mo-Bi-Ag)-(W-Sn)-(Pb-Zn-Cu),垂向分带序列为(Mo-Ag-Pb-Zn)-Cu-(Bi-W-Sn),并以w(Mo)/[w(Bi)×100]≥65,[w(Pb)×w(Zn)/w(W)×w(Sn)]≥25为判别标志,来预测深部盲矿体的存在。     

河南省栾川县罗村钼矿成矿特征及找矿

通过对河南省栾川县罗村钼矿区域地质背景、矿床地质特征与南泥湖、三道庄及东沟超大型钼矿的综合对比、分析、研究,总结归纳了矿区NWW构造形迹、小岩体与钼矿成矿关系、围岩对成矿的控制作用、围岩蚀变与成矿的关系、地球化学异常与钼矿床的关系等成矿特征.根据罗村钼矿的成矿特征,初步指出今后的找矿方向.     

海洋沉积物中的钒、钼、铊、镓及其环境指示意义

研究探讨沉积物中钒、钼、铊和镓的生物地球化学行为对揭示海洋环境演变机制有重要的科学意义,基于此考虑,本文系统分析总结了近年来海洋沉积物中V、Mo、Tl和Ga的地球化学特征以及与环境关系的研究进展,以期对深入开展环境敏感微量元素的海洋生物地球化学有所裨益。结果表明,由于受人为输入的影响,近海沉积物中V、Mo、Tl和Ga含量高于远海,河口高于近海;在表层沉积物中,细颗粒沉积物中V、Mo、Tl和Ga含量高于粗颗粒中的,且其含量与物源、有机质含量等沉积环境因素密切相关;在垂直分布上,随沉积物深度的增加,V、Mo、Tl和Ga含量趋于降低,表明近几十年来,随人为影响的加剧,海洋作为地球上物质的汇获得了比以前更多的V、Mo、Tl和Ga。由此可见,在水平方向上,海洋沉积物中V、Mo、Tl和Ga的丰度可表明输入物源的特性,而在柱状样中的垂直分布,则能够表征历史年代上V、Mo、Tl和Ga沉积量的差异。由于沉积物中V、Mo、Tl和Ga的性质比较稳定,它们在一定程度上可以揭示和表征海洋环境演变的讯息,追溯海洋环境演变的历史以及预测将来的发展趋向。     

河套地区土壤矿物组成分析及与各元素的关系

通过对河套地区土壤中矿物组成的分析研究,土壤中矿物组成中砂质成分主要为石英、长石、方解石,黏土矿物组合主要为伊利石、绿泥石和高岭石,此外还有角闪石等少量矿物成分。在砂土、粉砂土中石英、长石含量较高,在黏土质为主的土壤中黏土矿物含量增加。黏土矿物与石英以及长石呈负相关关系,与大多数元素呈明显正相关关系,黏土矿物对各元素具有明显吸附性;石英、长石与各元素含量呈负相关关系,说明其对元素不具有吸附性。     

The composition and age of the Argillite Sequence (sedimentary cover of the continental slope, Sea of Japan)

The Argillite Sequence located at the base of the sedimentary cover on the continental slope of the Sea of Japan was studied by petrographic, palynological, and X-ray diffraction methods. Two spores-pollen complexes were distinguished in it: the Late Oligocene reflecting cooling and the Early Miocene corresponding to initiated warming. The data obtained indicate that the sequence is composed of terrigenous silty-clayey sediments that accumulated in shallow coastal-marine settings. The global sea-level rise at the Early-Middle Miocene transition, combined with the regional tectonic processes, determined the basin deepening, owing to which the argillite sequence was overlain by thick Middle Miocene diatomaceous-clayey sediments. Due to tectonic movement along existing faults in the terminal Late Miocene, the argillite sequence occurring initially at depths of at least 400–500 m was locally exhumed to the basin bottom.     

Characterization of an Area Polluted by Copper and Zinc:the Relation between Soil Texture,Mineralogy and Pollutant Concentration

Abstract: Twenty-four soil samples were collected at three depths from an approximately 2.5 acre contaminated site in southern Piedmont (Italy) and then analyzed. The main soil parameters determined were: pH, Cation Exchange Capacity (CEC), particle size distribution, total organic carbon (TOC) content and retained metal concentration. The mineral phases were identified by X-Ray Powder Diffraction (XRPD). All of the samples contained Zn and Cu resulting from industrial contamination during the last century, and those obtained at depths of 20-40 cm consistently showed the highest levels. To determine which size fraction was most active in the retention process, the samples were separated into four fractions (≤2 mm, ≤63 μm, ≤30 μm and ≤2 μm) and the amount of pollutant measured in each. It was found that metal retention was the highest in the clayey fraction, whose clay minerals were identified by XRPD after K+ and Mg2+ saturation, glycerol treatment and heating to 550°C. The clayey fraction was also the richest in TOC, and a direct correlation between TOC amount and metal retention was observed.     

苏北梁王城遗址黄泛层初步研究

基于黄河下游流域考古遗址中第一次发现的黄泛地层,对苏北梁王城遗址T3902探方南壁剖面上部自然淤积层采样,结合考古断代,并参照历史资料,通过分析重砂矿物和粒度两方面的实验结果,揭示出考古遗址中黄泛地层的沉积物特征。旨在为今后环境考古中对黄泛地层的判别和对比提供可靠的科学依据,特别是为在黄河下游洪泛区考古遗址中疑似黄泛层的确认提供依据。