试论全国分布式水文数据库网络系统

试论全国分布式水文数据库网络系统王福炎，戴俊明（水利部水利信息中心）（河海大学计算机系）建设全国分布式水文数据库，是水文现代化的重要基础建设项目之一。其目标是，将水文系统内分散在全国各地的计算机资源，通过通信线路连接成网，在分布式数据库系统的支撑下，...     

江苏水文现代化探析

本文从全面推进江苏水利现代化、解决三大水问题、实现水文自身可持续发展等三个方面论述了加快推进江苏水文现代化建设的重要性和紧迫性，提出新时期江苏水文现代化建设的基本内涵是坚持“六个创新”，并结合江苏实际，提出当前水文现代化建设中突出抓好的“六个重点任务”。     

第一次全国水利普查与全国水文统计年报数据对比分析研究

通过对第一次全国水利普查中河湖基本情况普查、行业能力建设情况及全国水文统计年报数据的作用、目的、范围、方法和指标体系等进行对比研究,进一步分析了水利普查与统计年报工作的关系,有助于帮助水文统计人员进一步认识和理解水利普查与水文统计年报的工作衔接问题。     

宁夏水文计划管理信息系统建设探讨

根据水利部确立的以水利信息化带动水利现代化的发展思路,为了加快水文现代化建设,水文 计划管理信息系统的建设势在必行,本文提出了宁夏水文计划管理信息系统建设的规划     

对开展水文部门主要领导岗位培训教育工作的探讨

最近,杨振怀部长指出:“水利是基础产业,水文是水利的基础;整个水利系统要加强前期工作,水文是重点;科技兴水,进行现代化技术改造,要从水文开始;……”这一指示标志着水文事业面临新的形势,并将进入一个新的历史阶段。切实加强水文职工队伍的自身建设,适应形势的发展,是当前十分迫切的工作。对广大水文职工的培训、教育,是其中很重要的一个方面。     

水利现代化的内涵及评价指标体系的建立

立足于建立具有中国特色的水利现代化,考虑到地区间经济社会发展的不平衡和科技水平较低的现状,在借鉴国际上现代化标准和国内其他部门现代化水平的基础上遵循科学、实用及简明的原则,构建水利现代化评价指标体系,探索性地提出了水利现代化发展阶段的划分标准。     

我国水文资料整编和数据库技术发展综述

水文是水利和国民经济建设与发展重要的基础工作。经过整编的水文资料是国家重要的基础信息资源之一, 它被广泛应用于防汛抗旱、水工程规划设计、水资源管理与开发利用、水环境保护、水科学研究及其他国民经济建设。长期以来,水文资料为我国水利和国民经济建设与发展提供了科学决策依据。随着经济社会发展和人民生活水平不断提高,对控制水旱灾害、水环境监测与保护、水土保持与生态、水资源管理等方面要求越来越高,对水文资料分析处理、存储、应用服务要求也相应提高。本文主要从技术角度,对我国水文资料整编主要技术方法和水文年鉴发展进行了总结与分析;对水文数据库有关技术标准制定、水文数据库建设成就进行回顾;同时结合水文信息共享和应用服务需求,对相关技术发展进行了展望。     

吉林省城市生态建设现状评价及对比分析

建设生态经济城市是吉林省建设生态省过程中的一项重要内容,对我省国民经济和社会发展具有重要作用和意义。本文针对吉林省各主要城市生态建设的基础条件和实际情况,采用层次分析方法构建了包含生态经济、生态环境、社会发展3个子系统32个评价指标因子在内的评价指标体系。应用模糊综合评判法和综合指数法对吉林省9个主要城市从经济水平、产业结构等方面进行了生态建设现状评价,从而为城市生态建设规划等科学决策提供理论依据。     

建立水文标准化管理系统的可行性探讨

水文标准化工作是一项非常重要的水利基础设施建设工作。建立水文标准化管理系统以现代化、科学化、规范化管理为指导,强化标准在生产、建设和工作过程中的基础作用和主导作用、提升标准化管理工作的水平和效率,进一步提高标准的制修订水平,加快和完善标准化管理体系。     

基于可持续水文利用的恩施水资源承载力分析

结合恩施市水资源时空分布特征,在已有研究成果和指标选取原则标准上,基于水文的可持续利用标准构建了湖北省恩施市的水资源承载力评价指标体系,通过搭建水资源评价标准,采用模糊综合评价法对恩施水资源承载力进行了综合评估,并对未来恩施需水量做出了预测。研究表明:恩施市整体水资源利用处于较差水平,其水资源压力较大,评价结果与恩施市水资源承载力实际状况具有较高的吻合度,为该区域人水和谐建设和可持续水文利用提供借鉴。     

The terrestrial fauna of the Late Triassic Pant-y-ffynnon Quarry fissures,South Wales,UK and a new species of Clevosaurus (Lepidosauria: Rhynchocephalia)

Pant-y-ffynnon Quarry in South Wales yielded a rich cache of fossils in the early 1950s, including articulated specimens of new species (the small sauropodomorph dinosaur Pantydraco caducus and the crocodylomorph Terrestrisuchus gracilis), but no substantial study of the wider fauna of the Pant-y-ffynnon fissure systems has been published. Here, our overview of existing specimens, a few described but mostly undescribed, as well as freshly processed material, provides a comprehensive picture of the Pant-y-ffynnon palaeo-island of the Late Triassic. This was an island with a relatively impoverished fauna dominated by small clevosaurs (rhynchocephalians), including a new species, Clevosaurus cambrica, described here from a partially articulated specimen and isolated bones. The new species has a dental morphology that is intermediate between the Late Triassic Clevosaurus hudsoni, from Cromhall Quarry to the east, and the younger C. convallis from Pant Quarry to the west, suggesting adaptive radiation of clevosaurs in the palaeo-archipelago. The larger reptiles on the palaeo-island do not exceed 1.5?m in length, including a small carnivorous crocodylomorph, Terrestrisuchus, and a possible example of insular dwarfism in the basal dinosaur Pantydraco.     

Définition d'une limite multicritère ; stratigraphie du passage Campanien–Maastrichtien du site géologique de Tercis (Landes,SW France)Definition of a multi-criteria boundary; stratigraphy of the Campanian–Maastrichtian interval of the geological site at Tercis (Landes,SW France)

Lithostratigraphy, physicochemical stratigraphy, biostratigraphy, and geochronology of the 77–70 Ma old series bracketing the Campanian–Maastrichtian boundary have been investigated by 70 experts. For the first time, direct relationships between macro- and microfossils have been established, as well as direct and indirect relationships between chemo-physical and biostratigraphical tools. A combination of criteria for selecting the boundary level, duration estimates, uncertainties on durations and on the location of biohorizons have been considered; new chronostratigraphic units are proposed. The geological site at Tercis is accepted by the Commission on Stratigraphy as the international reference for the stratigraphy of the studied interval. To cite this article: G.S. Odin, C. R. Geoscience 334 (2002) 409–414.     

The effect of water on accessory phase solubility in subaluminous and peralkaline granitic melts

The solubilities of columbite, tantalite, wolframite, rutile, zircon and hafnon were determined as a function of the water contents in peralkaline and subaluminous granite melts. All experiments were conducted at 1035 °C and 2 kbar and the water contents of the melts ranged from nominally dry to approximately 6 wt.% H₂O. Accessory phase solubilities are not affected by the water content of the peralkaline melt. By contrast, solubilities are affected by the water content of the subaluminous melt, where the solubilities of all the accessory phases examined increase with the water content of the melt, up to 2 wt.% H₂O. At higher water contents, solubilities are nearly constant. It can be concluded that water is not an important control of accessory phase solubility, although the water content will affect diffusivities of components in the melt, thus whether or not accessory phases will be present as restite material. The solubility behaviour in the subaluminous and peralkaline melts supports previous spectroscopic studies, which have observed differences in the coordination of high field strength elements in dry vs. wet subaluminous granitic glasses, but not for peralkaline granitic glasses. Lastly, the fact that wolframite solubility increases with increasing water content in the subaluminous melt suggests that tungsten dissolved as a hexavalent species.     

Quaternary stresses revealed by calcite twinning inversion: insights from observations in the Savonnières underground quarry (eastern France)

Calcite samples were extracted both from the rock matrix and the superficial coating of a karstified fault plane of an underground quarry, located in the eastern border of the Paris basin. The karstification is dated as Quaternary. Analysis of mechanical calcite twinning reveals that only the calcite matrix has also undergone a compression trending WNW that can be attributed to the Mio-Pliocene alpine collision. Both coating and matrix have undergone a strike-slip regime with σ₁ roughly trending north–south, that could correspond to the regional present-day state of stress, a strike-slip compression rather trending NNW, modified by local phenomena. To cite this article: M. Rocher et al., C. R. Geoscience 335 (2003).     

NONMETALS DEPOSITS

正20141520 Bo Ying(Key Laboratory of Metallogeny and Mineral Assessment,MLR,Beijing 100037,China);Liu Chenglin Saline Spring Hydrochemical Characteristics and Indicators for Potassium Exploration in Southwestern and Northern Tarim Basin,Xinjiang(Acta Geoscientica Sinica,ISSN1006-3021,CN11-3474/P,34(5),2013,p.594-602,5 illus.,3 tables,28 refs.)     

MATHEMATICAL GEOLOGY

正20141243Chen Ge(Hangzhou Research Institute of Petroleum Geology,PetroChina,Hangzhou 310023,China);Si Chunsong Study on Sedimentary Numerical Simulation Method of Fan Delta Sand Body(Journal of Geology,     

PROSPECTING EXPLORATION

正20142599Chen Sanming(Guangxi Key Laboratory of Concealed Deposits Exploration,Guilin University of Technology,Guilin541004,China);He Yuzhou Block Model and Reserves Estimation of Panzhihua Iron Deposit Based on 3D Geological Modeling(Journal of Guilin University of Technology,ISSN1674-9057,CN45-1375/N,33(4),2013,p.610-615,9illus.,1table,15refs.)     

STRUCTURAL GEOLOGY

正20140594 Bai Daoyuan(Hunan Institute of Geology Survey,Changsha 410016,China);Zhong Xiang Faults in the Jingzhou Basin and Their Tectonic Settings(Geotectonica et Metallogenia,ISSN1001-1552,CN44-1595/P,37(2),2013,p.173-183,6illus.,59refs.)Key words:basin evolution,tectonic setting,South China In the Upper Paleozoic and Jurassic se-     

STRUCTURAL GEOLOGY

正20141912Cao Hui(State Key Laboratory for Continental Tectonics and Dynamics,Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China)Gravitational Collapse and Folding during Orogenesis:A Comparative Study of FIA Trends and Fold Axial Plane Traces(Geology in China,ISSN1000-3657,CN11-1167/P,40(6),2013,p.1818-1828,9illus.,35refs.,with