全文获取类型
收费全文 | 8281篇 |
免费 | 2327篇 |
国内免费 | 3335篇 |
专业分类
测绘学 | 1410篇 |
大气科学 | 1342篇 |
地球物理 | 1753篇 |
地质学 | 5413篇 |
海洋学 | 1914篇 |
天文学 | 110篇 |
综合类 | 715篇 |
自然地理 | 1286篇 |
出版年
2024年 | 81篇 |
2023年 | 207篇 |
2022年 | 588篇 |
2021年 | 655篇 |
2020年 | 577篇 |
2019年 | 664篇 |
2018年 | 582篇 |
2017年 | 516篇 |
2016年 | 533篇 |
2015年 | 623篇 |
2014年 | 585篇 |
2013年 | 723篇 |
2012年 | 832篇 |
2011年 | 777篇 |
2010年 | 851篇 |
2009年 | 742篇 |
2008年 | 720篇 |
2007年 | 683篇 |
2006年 | 714篇 |
2005年 | 558篇 |
2004年 | 398篇 |
2003年 | 303篇 |
2002年 | 269篇 |
2001年 | 273篇 |
2000年 | 229篇 |
1999年 | 84篇 |
1998年 | 33篇 |
1997年 | 18篇 |
1996年 | 18篇 |
1995年 | 5篇 |
1994年 | 12篇 |
1993年 | 7篇 |
1992年 | 6篇 |
1991年 | 8篇 |
1990年 | 12篇 |
1989年 | 2篇 |
1988年 | 3篇 |
1987年 | 7篇 |
1986年 | 3篇 |
1985年 | 4篇 |
1984年 | 5篇 |
1983年 | 2篇 |
1982年 | 3篇 |
1979年 | 9篇 |
1978年 | 1篇 |
1977年 | 1篇 |
1976年 | 3篇 |
1973年 | 1篇 |
1957年 | 7篇 |
1954年 | 6篇 |
排序方式: 共有10000条查询结果,搜索用时 390 毫秒
641.
按新旧规范设计的多层住宅砖房地震易损性的对比 总被引:1,自引:0,他引:1
本文采用概率方法借助于拉丁超立方采样技术和非线性地震反应时程分析对按现行规范设计的多层住宅砖房的地震易损性进行分析,并与按上一代规范设计的多层住宅砖房的地震易损性分析结果[1]进行了比较,为进一步研究这类结构的地震安全性、未来地震的损失预测以及防震减灾对策奠定基础。 相似文献
642.
为了达到快速、准确、可靠的围岩分类,有效指导隧道施工,在充分研究和吸取国内外有关围岩分类的经验和成果基础上,针对隧道施工期间的围岩类别鉴定方法,提出了一种可用于隧道施工期间围岩类别鉴定的快速分类方法,该方法以定量与定性相结合、多专家评分的方式在开挖掌子面现场进行观察、量测及评价,无需复杂试验或测量以及繁杂计算,可迅速得出评价结果。为了更加全面地反映隧道围岩情况,准确评价围岩工程性质,结合目前国际上流行的Q分类系统,在富溪隧道第一手实测资料的基础上,根据快速分类结果和Q指标分类结果对富溪隧道围岩条件进行综合评价,为其隧道施工提供了合理的支护参数。 相似文献
643.
644.
新疆可持续协调发展动态分析与评价 总被引:2,自引:0,他引:2
作为“资源大区”的新疆,在中国经济发展中具有重要的资源战略地位、生态安全地位和沿边开放地位。实施可持续发展战略,走可持续发展之路,是新疆区域发展的必然要求。在构建区域可持续发展指标体系的基础上,依据1980-2003年的统计数据,采用组合评价法研究新疆可持续协调发展及其动态变化,并得出一些主要结论和启示。 相似文献
645.
646.
Niobium and Ta concentrations in ultrahigh‐pressure (UHP) eclogites and rutile from these eclogites and associated high pressure (HP) veins were used to study the behaviour of Nb–Ta during dehydration and fluid‐rock interaction. Samples were collected through a ~2 km profile at the Bixiling complex in the Dabie orogenic belt, Central‐Eastern China. All but one eclogite away from veins (EAVs) display nearly constant Nb/Ta ratios ranging from 16.1 to 19.2, with an average of 16.9 ± 0.8 (2 SE), similar to that of their gabbroic protolith from the Yangtze Block. Nb/Ta ratios of rutile from the EAVs range from 12.7 to 25.3 among different individual grains, with the average values close to those of the corresponding bulk rocks. These observations show that Nb and Ta were not significantly fractionated by prograde metamorphism up to eclogite facies when no significant fluid‐rock interaction occurs. In contrast, Nb/Ta ratios of rutile from eclogites close to veins (ECVs) are highly variable from 17.8 to 49.8, which are systematically higher (by up to 17) than those of rutile from the veins. These observations demonstrate that Nb and Ta were mobilized and fractionated during localized fluid flow and intensive fluid‐rock interaction. This is strongly supported by Nb/Ta zoning patterns in single rutile grains revealed by in situ LA‐ICP‐MS analysis. Ratios of Nb/Ta in the ECV‐hosted rutile decrease gradually from cores towards rims, whereas those in the EAV‐hosted rutile are nearly invariable. Furthermore, the vein rutile shows Nb/Ta zoning patterns that are complementary to those in rutile from their immediate hosts (ECVs), suggesting an internal origin for the vein‐forming fluids. The Nb/Ta ratios of such fluids evolved from low values at the early stage of subduction to higher values at later supercritical conditions with increased temperature and pressure. Quantitative modelling was conducted to constrain the compositional evolution of metamorphic fluids during dehydration and fluid‐rock interaction focusing on Nb–Ta distribution. The modelling results based on our proposed multistage fluid phase evolution path can essentially reproduce the natural observations reported in the present study. 相似文献
647.
WEI ZHONG JIAYUAN CAO JIBIN XUE JUN OUYANG HAIMEI WANG XIAOHONG TANG XIAOYAN GAO 《Boreas: An International Journal of Quaternary Research》2012,41(1):102-112
Zhong, W., Cao, J., Xue, J., Ouyang, J., Wang, H., Tang, X. & Gao, X. 2012 (January): Carbon isotope evidence of last glacial climate variations in the tropical NW Leizhou Peninsula, South China. Boreas, Vol. 41, pp. 102–112. 10.1111/j.1502‐3885.2011.00224.x. ISSN 0300‐9483. Bulk organic δ13C values of sediment sequences are commonly used to indicate past climatic changes, although the causes and mechanisms leading to the observed organic carbon isotope responses are presently not fully understood. Based on two sedimentary sequences, namely a peat profile and a fluvial and swamp sequence from the tropical NW Leizhou Peninsula in South China, we interpret more negative bulk organic δ13C values to suggest wetter and warmer conditions, implying a stronger East Asian (EA) summer monsoon, and less negative δ13C values to indicate drier and cooler conditions, reflecting a weakening of the EA summer monsoon. A warm and wet period occurred between c. 48.0 and 28.0 cal. ka BP. In the study region, a climate shift occurred at c. 22.0 (or 20.0) cal. ka BP, and the driest and coldest period occurred between c. 19.0 and 16.0 cal. ka BP. After c. 12.0 cal. ka BP, the climate changed towards wetter and warmer conditions. Several possible millennial‐scale dry and cold oscillations characterized possibly by C4 plants, or by more positive organic δ13C values during the period when C3 plants dominated, are cautiously and tentatively interpreted as showing a similarity with Heinrich events and other cold millennial‐scale oscillations evidenced from a Greenland ice core and Chinese stalagmite. We demonstrate that bulk organic δ13C records of sedimentary sequences in the study region have potential for indicating the changes in vegetation composition that were closely associated with climate variation during the last glacial period. 相似文献
648.
A documental database of Papers in Chinese Seismological Journals (Englishedition)(高树心)(¥宋利萍)AdocumentaldatabaseofPapersinChi... 相似文献
649.
TheabnormalmantleanddeeptectonicprocessinthesouthernregionofNorthChinaPlainShi-YuGAO(高世玉),Hong-XiangHU(胡鸿翔)andShanDING(丁山)(In... 相似文献
650.
本文对比分析了各大地构造学说的特点,认为在地球的各种运动形式中,最重要的是地球的自转。地球在其运动中由于向心力和离心力联合力场作用的结果而形成各个圈层,地球表面形态和各圈层的物质在其旋转过程中发生不同形式的运动,而出现各种地质构造现象及相关的自然现象,诸如大气的流动、海水的进退、岩石的形变、地幔物质运动、各层圈物质交换与变化等等。在地球发展演化过程中,地壳的结构和构造也发生了一系列的变化,板块、构造体系、地槽、地洼、断块、大地波浪等大地构造形迹都是由于地球自转中地壳运动的结果。各种地质现象相互联系的总体,称之谓地质体系。 相似文献