创新是永恒的话题

创新是人类社会发展的原动力。江泽民同志指出：“创新是一个民族进步的灵魂，是国家兴旺发达的不竭动力”。科技期刊是反映一个国家科学技术创新、知识创新水平的窗口，是衡量一个国家科技水平与经济文化发展水平的重要标志。据统计，科技创新知识的的信息源70％以上来自科技期刊，有的学科领域则高达90％以上，同时科技期刊也是创新知识扩散与传播的主渠道。[第一段]     

地球科学的书目参考系统

地球科学的书目参考系统科技文献是科学技术研究成果的重要记录，也是科技发展的标志。随着科学技术的迅速发展，科技文献与日俱增，浩如烟海。在８０年代内，地球科学的文献以每年６７４８６篇的速率增长，这种文献增长水平对于地球科学家是一个不可忽视的问题。只有依靠...     

水文科技发展回顾及思考

水文科技是水文工作和水利科技一个重要组成部分,长期以来水文科学技术对我国水文与水利事业的发展和国民经济建设起到了巨大的推动作用,我国水文科学技术发展随着水文、水利与国民经济的发展和科学技术的进步取得了巨大成就,有些技术达到获接近国际先进水平。本文对我国水文科技取得的主要成就进行了总结,对目前水文科技存在主要问题进行了分析;结合水资源可持续利用支持社会经济可持续发展的需求,对水文科技发展的重点和策略进行了分析和探讨。     

发挥专利作用 推动地质科技进步——地矿系统专利工作

专利是世人掌握技术和经济竞争主动权的重要筹码,特别是在科技高速发展的今天,专利技术的拥有量在某种意义上反映了一个国家,部门或单位的科技水平。自1985年4月1日我国专利法实施以来,地矿系统的专利工作取得了较好的成绩,专利管理工作和专利服务工作体系也基本形成,专利法     

SCI源期刊中地学刊物科学评价指标介绍

SCI是美国科学信息研究所 ( ISI)编发的科学论文引用情况索引 ,现在已成为国际上较为通用的评定论文质量的一个重要指标。SCI的研究成果代表着世界基础科学研究的最高水准 ,一个国家科技论文被 SCI收录和引用 ,是评价该国的国际学术地位、基础科学研究水平 ,科技实力和科技论文质量高低的重要标准。由于多年来我国科技界对 SCI源期刊知之甚少 ,许多突破性科技创新成果仅发表在一些影响因子较低 ,不易被 SCI检索的学术期刊上 ,使得这些论文本应产生的巨大影响远远没有发挥出来。为了使地球科学界的科研人员了解 SCI源期刊中有关各项…     

中国地质大学(武汉)"211工程"学科建设成果

实施"211工程"是我国高等教育面向现代化、面向世界、面向未来,上水平、上质量、促改革、增效益、实施科教兴国的一个重大举措.这项工程的实施对提高我国高等教育水平,加快国家经济建设,促进科技水平的发展,增强综合国力和国际竞争能力,实现高层次人才培养立足于国内,将产生极其深远的影响.中国地质大学(武汉)是以学科建设进入"211工程"建设的,通过4年的建设有了较好的发展,取得了一批标志性成果,建设成效显著.     

加强地质科技档案管理及开发利用

目前，基层地勘单位的地质科技档案管理，还是比较落后的。从改善资料保管条件、改变档案管理模式、大力开发地质科技档案信息资源、管理人才的培养等几方面入手，论述了如何加强和提高地质科技档案管理水平，以及要重视对地质科技档案的开发利用等几个问题。     

矿物材料研究现状及发展前景

矿物材料研究成果和应用程度是衡量一个国家经济和科技的发达水平。在综述建筑、化工、冶金工业、机械工业、造纸工业、环境保护工业、农业、陶瓷业、电子光电工业等九个行业的矿物材料研究和应用状况的基础上,提出矿物材料在深加工、纳米矿物材料特性研究和新型矿物材料研制等的发展方向。     

通过国际科技论文统计分析看我国地质科研工作的态势

利用国际科技论文和中国科学院年报等统计资科，介绍了我国在国际上科技水平的地位，以及我国一些地质科研单位的研究水平状况，最后阐述了加强地质科研工作的一些措施。     

总结提高“六五”地质科技攻关成果在“七五”科技工作中取得更大成绩

“六五”期间,地矿部重点科技攻关项目的安排紧密结合地质-找矿任务,取得了显著的成果.反映出地矿系统确实有一支具有相当水平的科技队伍,有一批先进的技术装备,有一个比较完整的科研教育体系,也积累了一定的科技工作管理经验.同时也看到了我部地质科技的特点和优势,其特点体现在它的整体性与综合性,其优势在于技术     

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.     

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).     

HYDROGEOLOGY

正20141756 Chen Ruige(Mathematical College,China University of Geosciences,Beijing100083,China);Zhou Xun Numerical Simulation of Groundwater Level Fluctuation in a Coastal Confined Aquifer with Sloping Initial Groundwater Level Induced by the Tide(Geological Bulletin of China,ISSN1671-2552,CN11-4648/P,32(7),2013,p.1099-1104,6 illus.,16 refs.) Key words:confined water,groundwater level     

METAMORPHIC PETROLOGY

正20141408 Cai Jia(Institute of Geology,Chinese Academy of Geological Sciences,Beijing100037,China);Liu Fulai Petrogenesis and Metamorphic P-T Conditions of Garnet-Spinel-Biotitebearing Paragneiss in Danangou Area,Daqingshan-Wulashan Metamorphic Complex Belt(Acta Petrologica Sinica,ISSN1000-0569,CN11-1922/P,29(7),     

SERIALS

正~~     

GEOPHYSICAL EXPLORATION

正20142386An Guoying(China Aero Geophysical Survey and Remote Sensing Center for Land and Resources,Beijing 100083,China)Application of Satellite Remote Sensing in Regional Hydrogeological Investigation:Taking Cenozoic Strata in Wenquan Sheet(1∶250 000)of Karakoram Range as an Example(Geosci-     

QUATERNARY GEOLOGY & GEOMORPHOLOGY

正20141016An Chengbang(Key Laboratory of Western China’s Environmental Systems,Ministry of Education,Lanzhou University,Lanzhou 730000,China);Zhao Yongtao Lake Records during the Last Glacial Maximum from Xinjiang,NW China and Their Climatic Impli-     

PETROLEUM GEOLOGY

正20141538 Cao Qing(School of Earth Sciences and Engineering,Xi’an Petroleum University,Xi’an 710065,China);Zhao Jingzhou Characteristics and Significance of Fluid Inclusions from Majiagou Formation,Yichuan Huangling Area,Ordos Basin(Advances in Earth Science,ISSN1001-8166,CN62-1091/P,28(7),2013,p.819-828,7 illus.,3 tables,43 refs.)     

GEOCHEMISTRY

正20142002 Wei Hualing(Institute of Geophysical and Geochemical Exploration,Chinese Academy of Geological Sciences,Langfang065000,China);Zhou Guohua Element Content and Mineral Compositions in Different Sizes of Soil in Tongling Area,Anhui Province(Geological Bulletin of China,ISSN1671-2552,CN11-4648/P,32(11),2013,p.1861