溧阳震区地壳深部结构的探测与研究

本文利用天然地震转换波法所测得的漂阳震区地壳深部主要界面的构造图。简要地讨论了溧阳震区深部构造与震中分布的关系,认为溧阳两次中强地震都发生在较厚的花岗岩质层中,其深部构造特征表现为上地幔隆起、或界面埋深变化剧烈的梯度带,同时又处于两组以上深断裂交汇的特殊部位     

丹池盆地热水成因硅岩的沉积地球化学特征

丹池盆地硅岩（D₃1）属于典型的热水成因沉积物。它的显著地球化学特征之一是Sb.As和Ag富集,而REE贫乏,并且从近热水喷口→远离热水喷口,即沿着类碧玉岩→纹理状硅岩→块状泥质硅岩→硅页岩方向,元素、元素组合及稀土元素特征出现规律性的变化。     

云南大地热流及地热地质问题

本文报道了云南20多个大地热流测试数据。据热流分布特点并参考前人有关资料,结合地球物理测深资料、岩石热物性与放射性生热率测试数据,对各区地壳深度范围的温度、热流配分组成作了粗略分析,划分出各有特征的若干地质-热流区。云南普遍地热偏高(滇东南小范围除外)的主要原因是新构造运动强烈;怒江以西近代岩浆活动亦强烈,具有典型的板块交汇带的基本地热特点     

滇西北衙金矿矿床成因类型

滇西北衙金矿是一个曾被认为无工业价值的金矿，后在中科院地质与地球物理研究所蔡新平等（1989—2006年）科研成果的推动与促进下已成为一个具超大型远景规模的金矿床。文章简要介绍了北衙金矿的来历与研究概况，系统总结了北衙金矿的矿床类型及其结构模型。北衙金矿有3种成因不同的矿床，即与碱性斑岩有关的斑岩型和矽卡岩型Cu-Au矿床、与铁质热液或铁矿浆有关的Fe-Au矿床、及表生成因的Fe-Au矿床。北衙矿区复杂多样、多期叠加活动的岩浆与成矿作用，造就了矿区大规模的成矿作用。     

“江苏国土生态地球化学调查”项目分析测试成果验收获优秀

2005年12月23日~24日,中国地质调查局分析质量检查组对江苏省地质调查研究院测试所承担的“江苏国土生态地球化学调查”多元素分析测试工作进行了最终成果评审和评级验收。检查组听取了情况汇报,了解了数据的使用情况,随后逐一审阅了54项分析指标的地球化学图,同时对外部标准控制样的各项质量参数进行了统计分析,并查阅了分析测试的原始记录。检查组认为,“江苏国土生态地球化学调查”项目土壤样品多元素分析工作的各项指标均达到或优于规范要求,地球化学图图面效果好,元素空间分布规律与地质背景特征和生态环境特征相吻合,分析数据准确、可…     

宁波市鄞州建筑设计院

宁波市鄞州建筑设计院建院于1978年4月，具有国家甲级设计资质，承担工业与民用建筑设计、城乡规划、园林建筑、古建筑设计、岩土工程设计、勘察与检测、技术咨询、工程监理、工程装璜等。我院有较强的技术力量、经济实力和良好的社会信誉，现有注册资金210万元，建筑设计职工73名，技术人员69人，其中高级工程师13人，中级技术职称人员31人，注册建筑师15人，注册结构工程师16人。各专业技术人员配备齐全，级配合理。我院拥有办公建筑面积4800平方米，设计的技术装备达到宁波市先进水平，且有完善的计算机网络管理系统，并在1997年经宁波市CAD应甩工程示范点验收合格，我院还配备了正版的计算机设计软件，有效地保证了设计质量。     

神经网络技术及其在测井解释中的应用

在分析传统测井岩性解释中存在的一些问题的基础上，从神经网络的机理、特点出发，探讨了利用神经网络技术进行测井岩性识别的可行性及优越性，并以找矿目的层为对象，进行了岩性分析与对比，为该方法的进一步应用开拓了前景。     

Spatial analysis of elements in soils from Chengdu City

Three kinds of spatial analysis methods （geostatistics, concentration-area fractal model and the multifractal analysis called the moment method） were used for almost 50 elements, including heavy metals, disperse elements, rare elements and even others, in 6586 top soil （0-20 cm） samples and 1833 deep soil （150-200 cm） samples from Chengdu metropolitan area of 12400 km^2, southwestern China. The ranges of spatial correlation revealed by variograms are quite different for different kinds of elements in the top and deep soils. The most interest is the fact that the multifractal spectra of environmentally important elements such as Pb, Cr, Cd and Ni in top soils in the metropolitan area show systematic change from those in the deep soils, revealing a strong anthropogenic addition, while Hg, Zn, As, Cu and all common elements show no such kind of addition. In terms of multifractal properties based on the multifractal spectrum curves, those disperse and rare elements show great deviation from other major and trace elements, which is also of great interest.     

Measurement of the total nitrogen in lake sediments： Comparison and its environmental significance

Nitrogen cycle is an important bio-geochemical process in the environment. Measurement of the total nitrogen （TN） is a routine experiment in agriculture, biology and environmental sciences. The Kjeldahl method （KM） and elemental analyzer method （EA） are both commonly used to determine TN. Total nitrogen by EA is the sum of nitrate （NO3）, nitrite （NO2）, organic nitrogen and ammonia. Total nitrogen by KM （TKN） is made up of both organic nitrogen and ammonia. A comparative study focused on the two methods is conducted by analysis of TN in 97 samples from the sediment sequence of Gouchi, a salt lake in North China. KM presents a higher degree of accuracy than EA with a standard deviation of 0.007 vs. 0.024. With the presence of nitrate and/or nitrite nitrogen, however, measurement by KM is considerably lower than that by EA. Therefore, for samples from lake sediment sequences or soils in North China, KM is inapplicable to determining TN because of usually high contents of nitrous salt. Despite the inconsistency, use of both methods to the same samples makes sense in reconstructions of climatic and environmental changes from lake sediments. In Lake Gouchi, the contents of nitrate and nitrite nitrogen vary from 1.40% in the lower part of the sequence to 14.77% in the uppermost part, suggesting a gradual evolution process from a fresh water lake to the present-day salt lake.