全文获取类型
收费全文 | 28432篇 |
免费 | 897篇 |
国内免费 | 1967篇 |
专业分类
测绘学 | 1768篇 |
大气科学 | 2843篇 |
地球物理 | 5345篇 |
地质学 | 13514篇 |
海洋学 | 1637篇 |
天文学 | 1765篇 |
综合类 | 2525篇 |
自然地理 | 1899篇 |
出版年
2024年 | 24篇 |
2023年 | 79篇 |
2022年 | 214篇 |
2021年 | 281篇 |
2020年 | 216篇 |
2019年 | 256篇 |
2018年 | 4975篇 |
2017年 | 4234篇 |
2016年 | 2832篇 |
2015年 | 515篇 |
2014年 | 401篇 |
2013年 | 313篇 |
2012年 | 1265篇 |
2011年 | 2998篇 |
2010年 | 2270篇 |
2009年 | 2534篇 |
2008年 | 2098篇 |
2007年 | 2547篇 |
2006年 | 236篇 |
2005年 | 339篇 |
2004年 | 506篇 |
2003年 | 545篇 |
2002年 | 442篇 |
2001年 | 192篇 |
2000年 | 156篇 |
1999年 | 123篇 |
1998年 | 107篇 |
1997年 | 100篇 |
1996年 | 74篇 |
1995年 | 57篇 |
1994年 | 47篇 |
1993年 | 54篇 |
1992年 | 32篇 |
1991年 | 22篇 |
1990年 | 21篇 |
1989年 | 13篇 |
1988年 | 22篇 |
1987年 | 11篇 |
1986年 | 11篇 |
1985年 | 12篇 |
1984年 | 10篇 |
1983年 | 11篇 |
1982年 | 5篇 |
1981年 | 27篇 |
1980年 | 25篇 |
1977年 | 4篇 |
1976年 | 10篇 |
1975年 | 4篇 |
1972年 | 4篇 |
1971年 | 4篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
301.
青藏高原近地面层微气象学特征 总被引:12,自引:3,他引:12
Liu Huizhi Zhang Hongsheng Bian Lin'gen Chen Jiayi Zhou Mingyu Xu Xiangde Li Shiming Zhao Yijun 《大气科学进展》2002,19(1):73-88
利用1998年5月-7月在改则、当雄和昌都三测站获得的近地面层气象要素变化的观测资料,分析了青藏高原近地面层风速、温度和湿度日变化特征及廓线规律,发现高原近地面层微气象学特征具有自己的特点;同时还讨论了高原近地面层白天出现的逆湿现象。 相似文献
302.
通过引人泊松括号,分析了无限维Hamilton的性质,并将其推广到广义Hamilton系统,且从理论和实用角度讨论了这类广义Hamilton系统的辛格式构造问题,从而为辛几何算法在一般的时间发展方程的数值求解提供新的具体途径。 相似文献
303.
基于MAPGIS的军事标图系统的设计 总被引:2,自引:0,他引:2
军事领域是一个非常特殊的行业,信息的安全性和空间数据的多样性是应用开发的重要问题。在全球信息化日趋高速发展和逐步成熟的今天,军队信息化建设也必须与GIS技术紧密结合,跟上时代前进的步伐。较系统地研究了GIS技术在军事标图绘制中的应用和集成问题,并提供了相应的理论方法和实现系统。在此基础上介绍了以MAPGIS为开发平台的军事标绘系统的实用功能和特点。首先分析了军事信息系统对地理信息数据的要求,并且评述了相关领域的研究现状。然后较为系统地介绍了军事标图系统的总体设计,根据军事标绘对象的数据特征,设计符合要求的应用系统提出了面向对象和无缝交互工具等的设计思想。对军标对象数据模型和操作模型进行了详细地阐述和说明,并将这些模型在系统中进行了实现。最后介绍了军事标图系统的主要模块和功能,探讨了今后GIS研究和发展的方向。 相似文献
304.
长江三峡工程蓄水对链子崖危岩体T8-T12缝段稳定性影响研究 总被引:1,自引:1,他引:1
三峡水库蓄水后,已治理的链子崖危岩体,特别是T8-T12缝段岩体将受到江水的长期作用和影响,直接关系到防治工程的成败.通过大量实地调查和岩体测试,着重论述水库蓄水对T8-T12裂缝及其充填物的作用和影响;并以此为基础,用改进的Sarma法对该段危岩体的稳定性进行重新计算和评价,得出一系列新的结论:总体上,长江水位抬升后,水对裂缝的溶蚀作用和劈裂作用,使裂缝整体加宽,不利于危岩体的稳定;考虑岩体和承重阻滑键取长期强度和江水位骤然升降,以及地震影响,链子崖危岩体整体稳定性将恶化,但NE20°方向稳定程度好于NW350°. 相似文献
305.
云南银(铅)-锌矿开发史料与找矿探讨 总被引:1,自引:0,他引:1
云南是银铅锌矿开发较早的省份之一,史料丰富。本文从史料的角度,阐述了与云南古代有关银(铅)-锌矿的开发概况,基本特点以及如何保护,继承这份丰富的历史遗产,进而对目前有关史料的研究和古代采矿遗址清理情况进行分析,提出今后找矿的一些想法。 相似文献
306.
307.
The mode of occurrence of gold in the Yata micro-disseminated gold deposit is ap-proached through chemical phase studies coupled with ore-dressing monitoring and micro-beam analysis.The results showed that gold occurred for the most part as ultra-microscopic particles adsorbed on the surfaces or fracture planes of pyrite and other sulphides.The proportions of gold of different occurrences were estimated solutions containing nanometer-sized gold particles were prepared following the hydrolysis-reduction procedure and the adsorption of nanometer-sized gold on ordinary sulphides and rocks was experimentally determined.It is evident that sulphides are good adsorbents of gold and this is consistent with geological observations. 相似文献
308.
Victor Pinto Xavier Font Miquel Salgot Jose Tapias Tomas Mañá 《Environmental Geology》2002,41(5):495-503
One of the most important environmental impacts resulting from opencast mining, and especially quarries, is the visual impact. Evaluation of this impact considers two aspects: first, the area occupied by the quarry as seen by an observer from a specific place, and, second, the chromatic contrast existing between landscape and exploitation. In this study we develop a methodology to assess the chromatic impact in an objective and comparable form. To assess this impact we developed a method based on image analysis that allows us to obtain from a picture or image its equivalent as a function of chromatic impact, according to the sensibility of the human eye to different wavelengths. The methodology was applied to the Martinenca limestone quarry (Alcanar, Tarragona) and to Cerro Kori Kollo mine, La Joya district (Bolivia). 相似文献
309.
A. K. Varma R. M. Gairola A. K. Mathur B. S. Gohil Vijay K. Agarwal 《Journal of Earth System Science》2002,111(3):247-256
In this paper, MSMR geophysical products like Integrated Water Vapour (IWV), Ocean Surface Wind Speed (OWS) and Cloud Liquid
Water (CLW) in different grids of 50, 75 and 150 kms are compared with similar products available from other satellites like
DMSP-SSM/I and TRMMTMI. MSMR derived IWV, OWS and CLW compare well with SSM/I and TMI finished products. Comparison of MSMR
derived CLW with that derived from TMI and SSM/I is relatively in less agreement. This is possibly due to the use of 37 GHz
in SSM/I and TMI that is highly sensitive to CLW, while 37 GHz channels are not available on MSMR. Monthly comparison of MSMR
geophysical products with those from TMI is all carried out for climatological purpose. The monthly comparisons were much
better compared to instantaneous comparisons. In this paper, details of the data analysis and comparison results are presented.
The usefulness of the MSMR vis-à-vis other sensors is also discussed. 相似文献
310.
In the southern Pannonian Basin, the Variscan Barrovian- and overprinted Abukuma-type progressive metamorphic sequences of the South Tisia in Slavonian Mts. (SM) and Mt. Moslava)ka Gora (MG) are interlayered with orthoamphibolites. These sequences represent part of a disrupted Variscan belt that extends southeastwards of the Bohemian Massif through the Carpathians to the Caucasus. Orthoamphibolites contain hornblende (Mg-hornblende, tschermakite, pargasite, and edenite), plagioclase An48-98 (MG) and An26-35 (SM), biotite, grossular (MG) and almandine (SM) enriched garnet, diopside (MG), with accessory ilmenite, titanite, and clinozoisite. Based on major and trace element analyses and CIPW norms, these orthoamphibolites, which originally were olivine tholeiites to slightly alkalic basalts, can be correlated with tholeiites of consuming plate margins. '18O of orthoamphibolites varies from 5.8 to 7.1, the measured 87Sr/86Sr ratio from 0.70435 to 0.70665, which indicates slight continental crust contamination, and the calculated ratio from 0.70262 to 0.70535, indicating an upper mantle origin of the original basaltic melts. For associated penecontemporaneous I-type granitoids, the calculated initial 87Sr/86Sr ratio also have upper mantle values ranging between 0.70293 and 0.70368. Geochemical data for orthoamphibolites and the associated penecontemporaneous I-type granites, and the occurrence of alpine-type ultramafic bodies within the Barrovian sequence, indicate that they have many features in common with orogenic associations related to recent subduction-related settings. Some characteristic element ratios suggest back-arc basin environments and the Ce/K vs. Ce diagram suggests a pargasite-lherzolite source. Its partial melting gave primitive basaltic melts of olivine tholeiite to slight alkalic affinities that produced at first differentiated mafic rocks by olivine fractionation (future orthoamphibolites) and, afterwards, a strongly differentiated suite of I-type granitoids by amphibole fractionation. Magma emplacement and subsequent AFC processes took place in subduction environments preceding the main Variscan deformational metamorphic event during which orthoamphibolites were generated. This interpretation is compatible with geodynamic modeling of this part of the Paleotethys. 相似文献