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91.
中国城镇化发展的地理学贡献与责任使命 总被引:8,自引:4,他引:4
城镇化是中国全面建成小康社会和实现现代化的必由之路,中国城镇化不仅决定着中国的未来,而且决定着世界城镇化的进程。近35 a来中国地理学家对中国城镇化发展做出了重要贡献,主要表现在:首次提出了城镇化的概念,推动城镇化上升为国家战略;率先将Northam提出的城镇化发展三阶段论修正为四阶段论;提出了中国城镇化发展合理进程并被《国家新型城镇化规划》采用;研制了中国新型城镇化综合区划,构建了中国新型城镇化合理格局;率先研制了城镇化发展质量定量测度方法与系统,为提升城镇化发展质量提供了技术支撑;较早发布了《中国新型城镇化发展报告》,提出了新型城镇化发展的通用模式和差异模式;首次提出了城镇化与生态环境耦合圈理论与技术图谱。中国地理学家在城镇化这一多学科研究的重大领域中经常扮演着组织者角色,并担当重任,主要是:综合分析城镇化发展面临的问题及国际经验,探索城镇化发展的驱动机制与基本规律,辨析城镇化发展的空间格局和差异模式,揭示城镇化发展与资源环境的耦合关系,模拟预警城镇化发展的多种情景与风险,选择城镇化发展质量提升的可持续之路。今后一段时间内,创新国家新型城镇化高质量发展理论,优化“一带一路”背景下中国城镇化发展的空间格局,揭示中国城镇化与生态环境交互耦合机理及规律,研制中国城镇化发展的智能决策支持系统与引导政策,是中国城镇化发展的地理学使命。 相似文献
92.
管角螺Hemifusus tuba(Gmelin)稚贝在不同盐度下的生长和存活研究 总被引:1,自引:0,他引:1
在水温28.6—29.5℃、pH8.2条件下,研究了管角螺Hemifusus tuba稚贝[(壳高19.5±1.23)mm、体重(661.4±48.6)mg]在不同盐度下的生长和存活,并用二点法计算出最适宜存活和生长的盐度范围。结果表明,管角螺稚贝适宜存活盐度和最适存活盐度分别为17.7‰—40.8‰和25.1‰—35.9‰,适宜生长盐度和最适生长盐度分别为17.5‰—39.9‰和27.8‰—33.2‰。在最适生长盐度范围内,稚贝壳高日平均增长率为0.358—0.397mm.d 1,体重日平均增长率为44.64—49.09mg.d 1。超出上述范围,其存活率下降、生长率降低。稚贝在盐度17.0‰和41.3‰的海水中适应20d后再分别移至盐度14.0‰和45.0‰的海水中,72 h后存活率分别为84.0%和96.0%,而直接把生活在盐度为30.5‰中的稚贝放入到盐度为14.0‰和45.0‰的海水,72h后其存活率为8.0%和0,可见稚贝对盐度的适应能力与原生活海水盐度有关,经过驯化后的稚贝能够扩大对盐度的适应范围,提高对盐度的耐受力。 相似文献
93.
钟嘉芳 《广东海洋大学学报》2006,26(2):69-72
对赞文起源的了解。很大程度取决于对其字义的认识。“赞”字在上古有五种含义,最基本的意义为“助”、“明”.其它皆其引申之义。汉代“赞”义增加,有“赞美”之义。这是赞文发生转变的重要因索。赞发源很早.五帝时代已经产生,以口头形式主要用于三方面。祭典重赞、臣赞明事、释理托赞,有一定的实用价值,主要起“辅助”、“说明”作用.这决定了古赞具有依附性。 相似文献
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96.
With rapid urbanization and the socio-economic transformation,cultivated land protection has gradually become a major concern in China. The economic compensation plays a crucial role in promoting cultivated land protection and improving the utilization ratio of cultivated land. Farmer household's satisfaction has a great influence on the effectiveness of compensation. Therefore,households' willingness to select the economic compensation pattern for cultivated land protection has been considered and re-examined. By employing Participatory Rural Appraisal method (PRA),3 villages and 392 households were investigated and sampled in mesa and hilly areas of Chongqing. Then a quantitative analysis framework of household livelihood hexagon has been developed to quantify the livelihood assets of different farmer households. Finally,the Gray Relation Model and Probit Regression Model have been employed to explore the coupling relationship between the household livelihood assets and their compensation pattern options. The results show that there are both qualitative and spatial heterogeneity in household livelihood assets. We found that the inequality of livelihood assets is evident for five household types. There is a spatial trend that the higher the elevation,the less livelihood assets are. In addition,their options of economic compensation pattern vary from Chengdu Pattern to Foshan Pattern due to their difference in livelihood assets and difference in location. In detail,there is a coupling relationship between household livelihood assets and their compensation pattern;negative correlation is observed between natural assets value and household pattern options,while the other livelihood assets have positive impacts on compensation pattern in varying degrees,which from the top are psychological assets,human assets,physical assets,financial assets,and social assets respectively. A conceptual compensation pattern system has been designed to meet the demands for farmer households mainly according to their shortage in livelihood assets. In addition,compensation method,compensation standard,the basis of compensation and the source of compensation funds have been proposed accordingly. 相似文献
97.
中国区域经济增长差异研究进展与展望 总被引:4,自引:1,他引:3
缩小区域经济增长差异是中国区域经济发展的核心问题。本文从地理学和经济学的视角, 综合运用文献资料法、对比分析法, 评述了区域经济增长差异研究的进展, 分析了存在的主要问题, 并展望了下一步的研究重点与方向。结果表明:近年来国外研究在多学科融合框架下更为关注地理的作用, 从而导致空间计量分析和空间统计分析成为热点方法, 地理信息技术逐步受到重视, 研究尺度逐步降低并向实用化发展。国内研究多是国外经验在中国的验证, 本土化创新不足;研究尺度以省域层面为主, 城市和县域研究明显缺乏;空间效应逐步受到关注, 对区域差异的基本问题仍存在较大争议。未来研究应在数据选取上更为细化和全面, 尝试追踪和监测区域经济差异的动态变化格局, 构建经济增长差异定量测度方法体系和技术平台, 加强区域间的关联以及经济溢出、空间溢出效应测度研究, 关注差异机制和机理解析。 相似文献
98.
New Vetulicoliids from the Lower Cambrian Guanshan Fauna, Kunming 总被引:13,自引:3,他引:10
99.
Organic Geochemistry of Sedimentary Rock-hosted Disseminated Gold Deposits in Southwestern Guizhou Province, China 总被引:2,自引:1,他引:1
Jayanta GUHA 《《地质学报》英文版》2005,79(1):120-133
Sedimentary rock-hosted disseminated gold (SRHDG) deposits in the Youjiang-Nanpanjiang Basin,southwestem Guizhou Province are commonly hosted by the same fold crests that commonly contain a remarkable amount of organic material. The total organic carbon (TOC) contents of the ores and host rocks are usually less than 1%. The reflectance of vitrinite and pyrobitumen in the ores and the host rocks ranges from 1.5% to 4.5%, often in the range of 2% to 3%. In the Lannigou deposit, the reflectance of vitrinite and pyrobitumen in the ores is usually somewhat higher than those within the host rocks, indicating a hydrothermal impact on the organic matter in the altered host rocks. On the contrary, the estimated maximum paleotemperatures of the Getang and Zimudang deposits are higher than the homogenization temperatures of the fluid inclusions in the ores, signifying that the organic matter maturation predated Au mineralization. No correlation between the organic matter contents and Au concentrations were recognized in the ores.However, the most striking observation is that there is a positive correlation between the $2 (a parameter of Rock-Eval analysis), Au and As contents of the ores in the Lannigou deposit. Organic matter maturation and migration is apparent from the TOC vs. HCI diagram. Furthermore, group analysis of the dichloromethane extractable organic component of the ores and host rocks shows that the maturation degree of the organic matter in the ores is slightly higher than that of the host rocks in the Lannigou gold deposit. However, the compositions of their alkanes, steranes and terpenes, which serve as biomarkers, are quite similar; this suggests that the organic matter found in the ores and host rocks has a common marine source. Organic matter probably contributed to the preconcentration of Au in the host rocks. Hydrocarbons in the system,on the other hand, clearly contributed to the emplacement of the gold mineralization through thermal sulfate reduction.Organic matter in the solution might have increased the potential of the hydrothermal solution to transport Au. 相似文献
100.
根据收集到的日照市海岸带浅地层剖面测量调查资料,把多条浅地层剖面中出露的古河道断面推测性地连接起来,重建了以往的古河道体系,综合分析了日照市海岸带古河道的分布特征。日照近海区域存在一个主干河道呈SW-NE走向的梳状河道网,古河道形成于距今约4.4万a的末次冰期。古河道的形成是河流的侵蚀、搬运、沉积及后期的海平面上升、潮汐改造等多种因素共同作用的结果。在末次冰期,研究区内气候湿润,河流流速较大,河流搬运泥沙的能力较强,长期侵蚀作用形成下切古河道,在古河道中容易形成淤积较多河流携带的砂体。古河道断面形态主要呈U形、V形、W形、箱形和倒梯形。主干河道北西侧,分支河道较密,南东侧分支河道较稀疏。主河道长约40km,横截面由南西向北东逐渐变宽,最宽处达4km。分支河道多数以NW向为主,少数为NE向,长度介于8~20km之间,宽度约为1~3km。古河道主要位于16~24m水深的闭合深度以外区域,对其中的砂体经过粒度筛选可作为将来进行人工抛沙的砂源。 相似文献