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2012年12月12日,国际地质科学联合会主席Roland Oberhnsli教授与秘书长Ian Lambert教授在中国地质科学院副院长、国际地科联司库董树文教授的陪同下,应邀访问了中国地质科学院全球矿产资源战略研究中心。全球矿产资源战略研究中心主任王安建教授作了题为"全球矿产资源需求旺盛—国际地科联可以做得更好"的学术报告,报告包括能源与矿产资源消费的历史背景、能源与矿产资源消费的基本规律、未来20 相似文献
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本文以能源和大宗矿产资源消费与经济发展的"S"形规律为基础,总结并讨论了发达国家经济社会发展过程中,人均能源和矿产资源消费增长的极限及其与基础设施建设、城市化水平、社会财富积累以及经济结构变化的关系;指出人类对美好生活的物质追求是推动能源和矿产资源消费增长的原动力,从农业社会、工业社会到后工业化社会,随着经济发展,即人均收入或人均GDP的不断提高,城市化率、基础设施建设和社会财富积累水平持续提升,大宗商品或资源性产品消费将陆续进入准近饱和状态,消费结构的改变,致使铁、铜、铝等大宗矿产在工业化中期开始陆续到达人均消费极限值,并引起产业结构调整升级,推动经济结构变迁;进入后工业化发展阶段,以服务业为主体的国民经济体系逐渐使人均能源消费增长到达极限值;强调国家集团或大国资源消费增长极限的到来是导致全球性矿产资源消费增长周期结束的根本原因。 相似文献
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中国重要矿产资源的需求预测 总被引:18,自引:22,他引:18
以往对矿产资源的中长期需求预测,大都基于纯数学模型或情景分析对已有数据的经验外推。由于缺乏对工业化过程矿产资源消费需求基本规律的把握,预测结果几乎无一例外地存在巨大偏差。笔者在深入分析工业化经济增长与矿产资源消费需求的相关关系、基本规律和模式的基础上,探讨了工业化过程中矿产资源消费从怎样的初始值通过什么样的方式到达多高的峰值,进而提取经济增长与矿产资源消费需求的模式参数,预测了中国未来30a能源、钢、铜、铝、锌的消费需求。 相似文献
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对于不可再生的矿产资源,由于生产和消费的迅速增长,对其研究空前地加强了.人们对矿产资源问题的注意力从来没有像现在这样大.在德意志联邦共和国汉诺威市,每隔三年召开一次矿产资源问题国际学术讨论会.1976及1979年召开的前两次会议主要探讨了地球矿产资源的潜力及影响矿产资源应用的各种问题.最新一次,即1982年召开的第三次国际讨论会则以“矿产勘查的新途径”为主题,广泛讨论了矿产资源政策;能源资源及金属非金属矿物原料的普查、勘探与评价等问题.1985年将召开新的一次讨论会.这是一个引人注目的矿产资源问题国际研讨中心.会议的东道主,联邦地球科学及自然资源研究所及下萨克森州地质调查所所长本德尔教授在1982年会议闭幕词中说:“许多国家,不论是发展中国家或是工业化 相似文献
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工业部门作为终端能源消费中三大主要部门之一,对经济发展具有重要作用。本文系统分析了15个发达经济体100多年来工业部门终端能源消费与人口和经济发展(GDP)的关系,发现随着人均GDP的增长,工业部门的人均终端能源消费显现缓慢增长、加速增长、减速增长到零增长或负增长的"S"形轨迹,并可分为高、中、低三个类型。通过重点解剖美、日、德、法和意大利等典型国家工业部门终端能源消费与经济发展的历史,标定了不同类型"S"形曲线的起飞点、转折点和零增长点,讨论了工业部门终端能源消费与能源消费强度、二产比例、城市化率和人均钢铁消费的内在联系,建立了"S"形曲线的一般性数学模型。工业部门终端能源消费与经济发展定量关系的确定对于国家,特别是发展中国家把握工业化过程能源消费趋势、预测能源需求和制定相关能源政策具有重要意义。 相似文献
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【研究目的】近年来,全球经济产业结构和能源供给结构向绿色低碳转型,新能源产业加速发展。了解新能源背景下全球锂资源产业链发展现状和趋势,有助于为全球锂行业可持续发展提供基础性认识,为政府和企业提升锂资源产业链竞争力提供相关参考。【研究方法】本文梳理了日益增长的新能源需求对全球锂资源产业链在资源供需、冶炼加工、终端消费、回收利用等各环节的具体影响。【研究结果】通过梳理分析,新能源背景下全球锂资源终端消费,尤其是动力电池领域,持续旺盛,全球锂需求快速增长,供需错位下价格持续上升;锂资源在全球地位提升,世界各主要经济体将其列为关键矿产,出台系列政策保障本国锂资源安全供应、加强锂资源回收利用、推动产业结构转型升级;企业生产方式、企业结构、发展目标朝着低碳化、一体化、可持续方向发展。【结论】发展高效清洁能源成为世界各主要经济体解决能源和环境问题的有效途径,交通电力化和能源储存使全球对锂资源的需求持续快速增加。这些变化对上游锂矿产资源的供应格局,以及产业链中游生产加工和下游终端消费结构都产生了较大影响,但对产业链各环节传导和具体的影响方式是不均衡的。 相似文献
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Emily Keeble David I. Whiteside Michael J. Benton 《Proceedings of the Geologists' Association. Geologists' Association》2018,129(2):99-119
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. 相似文献
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The effect of water on accessory phase solubility in subaluminous and peralkaline granitic melts 总被引:4,自引:0,他引:4
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. 相似文献
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Muriel Rocher Stéphane Baize Stéphane Jaillet Edward Marc Cushing Yannick Lozach Francis Lemeille 《Comptes Rendus Geoscience》2003,335(8):701-708
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). 相似文献
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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 相似文献
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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), 相似文献
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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- 相似文献
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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- 相似文献
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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.) 相似文献
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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 相似文献