全文获取类型
收费全文 | 49924篇 |
免费 | 5253篇 |
国内免费 | 7429篇 |
专业分类
测绘学 | 2569篇 |
大气科学 | 7790篇 |
地球物理 | 11351篇 |
地质学 | 24931篇 |
海洋学 | 3995篇 |
天文学 | 2979篇 |
综合类 | 4756篇 |
自然地理 | 4235篇 |
出版年
2024年 | 136篇 |
2023年 | 541篇 |
2022年 | 1253篇 |
2021年 | 1430篇 |
2020年 | 1183篇 |
2019年 | 1286篇 |
2018年 | 5898篇 |
2017年 | 5062篇 |
2016年 | 3925篇 |
2015年 | 1553篇 |
2014年 | 1759篇 |
2013年 | 1576篇 |
2012年 | 2374篇 |
2011年 | 4049篇 |
2010年 | 3410篇 |
2009年 | 3674篇 |
2008年 | 3079篇 |
2007年 | 3444篇 |
2006年 | 1081篇 |
2005年 | 1067篇 |
2004年 | 1122篇 |
2003年 | 1169篇 |
2002年 | 989篇 |
2001年 | 744篇 |
2000年 | 974篇 |
1999年 | 1406篇 |
1998年 | 1142篇 |
1997年 | 1121篇 |
1996年 | 1015篇 |
1995年 | 883篇 |
1994年 | 831篇 |
1993年 | 698篇 |
1992年 | 546篇 |
1991年 | 438篇 |
1990年 | 324篇 |
1989年 | 304篇 |
1988年 | 268篇 |
1987年 | 171篇 |
1986年 | 150篇 |
1985年 | 114篇 |
1984年 | 70篇 |
1983年 | 58篇 |
1982年 | 71篇 |
1981年 | 77篇 |
1980年 | 51篇 |
1979年 | 31篇 |
1978年 | 10篇 |
1977年 | 4篇 |
1976年 | 13篇 |
1958年 | 27篇 |
排序方式: 共有10000条查询结果,搜索用时 17 毫秒
91.
煤层冲刷带预测方法评述 总被引:2,自引:0,他引:2
介绍了沉积分析法、矿井物探法以及地质统计法三种煤层冲刷带预测方法.实例证明,根据煤矿生产的具体情况,选择一种或综合运用几种方法,能较好地预测冲刷带的位置和范围. 相似文献
92.
Development of the ideas about the equilibrium between freshwater and saline water has received considerable attention in the literature, but little has been written so far about the earliest scientific works about well salinization. Based on a review of the literature from the second half of the 19th century and the early 20th century, this historical note explores how insights into groundwater abstraction and saltwater intrusion developed, and examples of the earliest field studies are provided. Fundamental research was driven by the need for increasing water supply, but the progress of science did not lead to sustainable management practices everywhere. Research outcomes were shared between scientists of different countries, marking the beginning of coastal hydrogeology as a scientific specialization in the first decade of the 20th century. 相似文献
93.
A reasonable warmer winter index (IWWI) in the framework of the three equiprobability categories (i.e. warmer, normal and colder categories) is proposed based on the winter temperature data observed at 565 stations in China during 1956-2005, where IWWI is defined as the ratio of the station number of warmer category over the total number of stations. The results suggest that the trend of IWWI was consistent with that of the winter temperature on decadal time scale, and their rates of change were 10%/10 a and 0.4 ℃/10 a, respectively. It is found that only 13 warmer winter events in total were detected by IWWI over the past 50 years, and 85% of them occurred after 1986. 相似文献
94.
95.
96.
对青海省五龙沟含碳、砷、硫、锑微细粒难选冶金矿石的浮选金精矿进行二段焙烧——焙砂氰化浸出提金的试验研究,获得了金浸出率89.90%的较好指标,为该矿山浮选金精矿的提金提供了一种可选择的工艺流程。 相似文献
97.
98.
Lin Ding Satybaev Maksatbek FuLong Cai HouQi Wang PeiPing Song WeiQiang Ji Qiang Xu LiYun Zhang Qasim Muhammad Baral Upendra 《中国科学:地球科学(英文版)》2017,60(4):635-651
The initial collision between Indian and Asian continents marked the starting point for transformation of land-sea thermal contrast, uplift of the Tibet-Himalaya orogen, and climate change in Asia. In this paper, we review the published literatures from the past 30 years in order to draw consensus on the processes of initial collision and suturing that took place between the Indian and Asian plates. Following a comparison of the different methods that have been used to constrain the initial timing of collision, we propose that the tectono-sedimentary response in the peripheral foreland basin provides the most sensitive index of this event, and that paleomagnetism presents independent evidence as an alternative, reliable, and quantitative research method. In contrast to previous studies that have suggested collision between India and Asia started in Pakistan between ca. 55 Ma and 50 Ma and progressively closed eastwards, more recent researches have indicated that this major event first occurred in the center of the Yarlung Tsangpo suture zone (YTSZ) between ca. 65 Ma and 63 Ma and then spreading both eastwards and westwards. While continental collision is a complicated process, including the processes of deformation, sedimentation, metamorphism, and magmatism, different researchers have tended to define the nature of this event based on their own understanding, an intuitive bias that has meant that its initial timing has remained controversial for decades. Here, we recommend the use of reconstructions of each geological event within the orogenic evolution sequence as this will allow interpretation of collision timing on the basis of multidisciplinary methods. 相似文献
99.
Magma underplating and Hannuoba present crust-mantle transitional zone composition: Xenolith petrological and geochemical evidence 总被引:7,自引:0,他引:7
FAN Qicheng ZHANG Hongfu SUI Jianli ZHAI Mingguo SUN Qian & LI Ni . Institute of Geology Geophysics Chinese Academy of Sciences Beijing China . Institute of Geology China Seismological Bureau Beijing China 《中国科学D辑(英文版)》2005,48(8):1089-1105
Studies on the deep-seated xenoliths from global volcanoes reveal that the present petrological crust-mantle boundary between the lower crust and the upper mantle actually is a transitional layer from mainly mafic granulites to ultramafic spinel lher-zolites[1,2], i.e. a transitional zone distinctive from the seismological Moho[3]. Oceanic lithosphere crust- mantle transitional zone can be established from the study on the exposed ophiolites. However, as for the continental lithosphere, since … 相似文献
100.
The structure of the mid- and high-latitude ionosphere during the November 2004 storm event obtained from GPS observations 总被引:1,自引:1,他引:1
Andrzej Krankowski Irk I. Shagimuratov Lubomir W. Baran Galina Yakimova 《Acta Geophysica》2007,55(4):490-508
GPS data from the International GNSS Service (IGS) network were used to study the development of the severe geomagnetic storm
of November 7–12, 2004, in the total electron content (TEC) on a global scale. The TEC maps were produced for analyzing the
storm. For producing the maps over European and North American sectors, GPS measurements from more than 100 stations were
used. The dense network of GPS stations provided TEC measurements with a high temporal and spatial resolution. To present
the temporal and spatial variation of TEC during the storm, differential TEC maps relative to a quiet day (November 6, 2004)
were created.
The features of geomagnetic storm attributed to the complex development of ionospheric storm depend on latitude, longitude
and local time. The positive, as well as negative effects were detected in TEC variations as a consequence of the evolution
of the geomagnetic storm. The maximal effect was registered in the subauroral/auroral ionosphere during substorm activity
in the evening and night period. The latitudinal profiles obtained from TEC maps for Europe gave rise to the storm-time dynamic
of the ionospheric trough, which was detected on November 7 and 9 at latitudes below 50°N. In the report, features of the
response of TEC to the storm for European and North American sectors are analyzed. 相似文献