全文获取类型
收费全文 | 3315篇 |
免费 | 575篇 |
国内免费 | 596篇 |
专业分类
测绘学 | 391篇 |
大气科学 | 260篇 |
地球物理 | 1063篇 |
地质学 | 1131篇 |
海洋学 | 303篇 |
天文学 | 1011篇 |
综合类 | 145篇 |
自然地理 | 182篇 |
出版年
2024年 | 21篇 |
2023年 | 59篇 |
2022年 | 92篇 |
2021年 | 113篇 |
2020年 | 129篇 |
2019年 | 148篇 |
2018年 | 107篇 |
2017年 | 130篇 |
2016年 | 164篇 |
2015年 | 177篇 |
2014年 | 192篇 |
2013年 | 164篇 |
2012年 | 174篇 |
2011年 | 167篇 |
2010年 | 161篇 |
2009年 | 249篇 |
2008年 | 224篇 |
2007年 | 275篇 |
2006年 | 246篇 |
2005年 | 193篇 |
2004年 | 198篇 |
2003年 | 173篇 |
2002年 | 140篇 |
2001年 | 134篇 |
2000年 | 102篇 |
1999年 | 100篇 |
1998年 | 107篇 |
1997年 | 33篇 |
1996年 | 59篇 |
1995年 | 41篇 |
1994年 | 32篇 |
1993年 | 38篇 |
1992年 | 26篇 |
1991年 | 24篇 |
1990年 | 28篇 |
1989年 | 15篇 |
1988年 | 18篇 |
1987年 | 13篇 |
1986年 | 4篇 |
1985年 | 4篇 |
1984年 | 1篇 |
1983年 | 1篇 |
1982年 | 2篇 |
1981年 | 1篇 |
1980年 | 1篇 |
1978年 | 1篇 |
1977年 | 1篇 |
1954年 | 4篇 |
排序方式: 共有4486条查询结果,搜索用时 15 毫秒
981.
982.
基于半解析模型和SDSS DR4(Sloan Digital Sky Survey Data Release 4),研究了环境对星系性质的影响.通过对以颜色、恒星形成率和恒星质量的带权重的相关函数的测量,发现半解析模型在颜色和恒星质量上与SDSS数据符合得比较好,而恒星形成率则在SDSS数据中表现为与环境无关.此结论证实了半解析模型对星系中部分性质与环境关系的预测,但对于恒星形成率为何与环境无关仍有待研究. 相似文献
983.
Gamma‐ray bursts (GRBs) are one of the most luminous events in the Universe. In addition, the Universe itself is almost transparent to γ ‐rays, making GRBs detectable up to very high redshifts. As a result, GRBs are very suitable to probe the cosmological parameters. This work shows the potential of long‐duration GRBs for measuring the cosmological parameters ΩM and ΩΛ by comparing the observed log N ‐log P distribution with the theoretical one. Provided that the GRBs rate and luminosity function are well determined, the best values and 1σ confidence intervals obtained are ΩM = 0.22+0.05–0.03 and ΩΛ = 1.06+0.05–0.10. Finally, a set of simulations show the ability of the method to measure ΩM and ΩΛ (© 2010 WILEY‐VCH Verlag GmbH & Co. KGaA, Weinheim) 相似文献
984.
985.
986.
987.
988.
989.
为了探索中国西南喀斯特地区石漠化过程中土壤物理性质的变异规律,采用野外采样与实验室分析相结合的方法,对贵州省荔波县及普定县不同石漠化阶段典型土壤的物理参数进行了研究。结果表明:土壤有机质质量分数随石漠化程度的加深逐渐减小;非石漠化土壤重度仅为6.15 N/m^3,随着石漠化的发展,土壤重度逐渐增大,总孔隙度随之减小;石漠化的发展导致土壤黏粒含量升高;土壤水稳性团聚体质量分数及微团聚体的结构系数均随石漠化程度加深而减小;土壤有机质质量分数与重度、砂粒含量、大于5 mm团聚体含量及结构系数的相关系数分别为-0.921 2、0.827 7、0.907 2、0.899 3,均达到极显著水平。通过封山育林等措施增加喀斯特地区有机质积累可改善土壤物理性质,对防治石漠化具有重要意义。 相似文献
990.
Moshood Niyi Tijani Matthew Essien Nton Ryuji Kitagawa 《Comptes Rendus Geoscience》2010,342(2):136-150
This study presents the mineralogical, textural and geochemical characteristics of the regional Maastrichtian Ajali Sandstone in Anambra Basin, SE Nigeria. The intent is to highlight possible constraints on the chemical weathering conditions of the source materials on one hand, and to infer the provenance on the other hand. The investigation approach involved field studies and collection of samples from 12 different outcrop locations, followed by laboratory studies involving grain-size analysis (GSA), major and trace elements analyses using the X-ray fluorescence (XRF) method as well as thin section petrography. Field studies show that the sandstones are friable at all locations and range in color from white in freshly cut stone, to reddish brown on weathering. In addition, the sandstone units are cross-bedded and show graded bedding exemplified by fining upward sequence. Textural examination indicates that the sandstones range from fine to medium sands, constituting about 76 to 99% sand fraction, with graphic mean grain size of 0.23 to 0.53 mm. Standard deviation (sorting) ranges from 0.56 to 1.24 Ø and implies moderately well sorted sediments. Inferred from the textural indices, the depo-environmental discrimination of the Ajali Sandstone revealed a fluvial/river system-dominated sedimentary process. The sandstones are quartz arenite with quartz greater than 90% and less than 5% K-feldspar which indicate a predominant basement source as also revealed by the heavy mineral assemblages. In addition, major elemental oxides shows SiO2 content greater than 96% for the fresh Ajali Sandstone samples with extreme depletion of mobile oxides such as Na2O, CaO and the ferromagnesian minerals through weathering and sedimentary processes. Provenance and tectonic setting discrimination using geochemical data and compositional maturity revealed typical felsic igneous-dominated cratonic environment while inter-elemental ratios (such as Zr/Cr, Y/Ni, Th/Sc, La/Sc and La/Co) and ternary plots (e.g. Th–Sc–Zr; La-Th–Sc and Th-Co-Zr) reflect passive continental margin setting for the Ajali Sandstone. Consequently, the source area is constrained to the Precambrian basement rock units of Adamawa-Oban massif areas to the east of the Anambra Basin and the adjacent Abakaliki Anticlinorium. 相似文献