全文获取类型
收费全文 | 2356篇 |
免费 | 689篇 |
国内免费 | 438篇 |
专业分类
测绘学 | 645篇 |
大气科学 | 358篇 |
地球物理 | 936篇 |
地质学 | 983篇 |
海洋学 | 258篇 |
天文学 | 26篇 |
综合类 | 193篇 |
自然地理 | 84篇 |
出版年
2024年 | 4篇 |
2023年 | 32篇 |
2022年 | 75篇 |
2021年 | 91篇 |
2020年 | 119篇 |
2019年 | 126篇 |
2018年 | 94篇 |
2017年 | 153篇 |
2016年 | 121篇 |
2015年 | 160篇 |
2014年 | 192篇 |
2013年 | 163篇 |
2012年 | 152篇 |
2011年 | 151篇 |
2010年 | 114篇 |
2009年 | 153篇 |
2008年 | 159篇 |
2007年 | 170篇 |
2006年 | 159篇 |
2005年 | 145篇 |
2004年 | 130篇 |
2003年 | 93篇 |
2002年 | 93篇 |
2001年 | 73篇 |
2000年 | 59篇 |
1999年 | 58篇 |
1998年 | 68篇 |
1997年 | 48篇 |
1996年 | 57篇 |
1995年 | 51篇 |
1994年 | 46篇 |
1993年 | 49篇 |
1992年 | 22篇 |
1991年 | 18篇 |
1990年 | 25篇 |
1989年 | 11篇 |
1988年 | 12篇 |
1987年 | 9篇 |
1984年 | 1篇 |
1983年 | 1篇 |
1981年 | 1篇 |
1980年 | 4篇 |
1979年 | 2篇 |
1978年 | 10篇 |
1977年 | 2篇 |
1954年 | 7篇 |
排序方式: 共有3483条查询结果,搜索用时 671 毫秒
61.
Seismic observations have shown structural variation near the base of the mantle transition zone(MTZ)where subducted cold slabs,as visualized with high seismic speed anomalies(HSSAs),flatten to form stagnant slabs or sink further into the lower mantle.The different slab behaviors were also accompanied by variation of the "660 km" discontinuity depths and low viscosity layers(LVLs) beneath the MTZ that are suggested by geoid inversion studies.We address that deep water transport by subducted slabs and dehydration from hydrous slabs could affect the physical properties of mantle minerals and govern slab dynamics.A systematic series of three-dimensional numerical simulation has been conducted to examine the effects of viscosity reduction or contrast between slab materials on slab behaviors near the base of the MTZ.We found that the viscosity reduction of subducted crustal material leads to a separation of crustal material from the slab main body and its transient stagnation in the MTZ.The once trapped crustal materials in the MTZ eventually sink into the lower mantle within 20-30 My from the start of the plate subduction.The results suggest crustal material recycle in the whole mantle that is consistent with evidence from mantle geochemistry as opposed to a two-layer mantle convection model.Because of the smaller capacity of water content in lower mantle minerals than in MTZ minerals,dehydration should occur at the phase transformation depth,~660 km.The variation of the discontinuity depths and highly localized low seismic speed anomaly(LSSA) zones observed from seismic P waveforms in a relatively high frequency band(~1 Hz) support the hypothesis of dehydration from hydrous slabs at the phase boundary.The LSSAs which correspond to dehydration induced fluids are likely to be very local,given very small hydrogen(H~+) diffusivity associated with subducted slabs.The image of such local LSSA zones embedded in HSSAs may not be necessarily captured in tomography studies.The high electrical conductivity in the MTZ beneath the northwestern Pacific subduction zone does not necessarily require a broad range of high water content homogeneously. 相似文献
62.
63.
平武地震台数字地震仪记录近震震级及定位偏差 总被引:2,自引:0,他引:2
以《四川省地震台网地震目录》作为地震定位参考标准,对平武地震台数字地震仪记录的近震,尤其是汶川"5·12"地震序列定位参数进行了对比。结果表明,平武单台数字地震仪记录得到的测定结果与《四川省地震台网地震目录》间存在一定程度的差异。这里给出了台站可以简单应用的偏差评估值和处理方法。 相似文献
64.
Stijn Hantson Emilio Chuvieco 《International Journal of Applied Earth Observation and Geoinformation》2011
The recent free availability of Landsat historical data provides new potentials for land-cover change studies. Multi-temporal studies require a previous radiometric and geometric homogenization of input images, to better identify true changes. Topographic normalization is one of the key steps to create consistent and radiometricly stable multi-temporal time series, since terrain shadows change throughout time. This paper aims to evaluate different methods for topographic correction of Landsat TM-ETM+ data. They were assessed for 15 ETM+ images taken under different illumination conditions, using two criteria: (a) reduction of the standard deviation (SD) for different land-covers and (b) increase in temporal stability of a time series for individual pixels. We observed that results improve when land-cover classes where processed independently when applying the more advanced correction algorithms such as the C-correction and the Minnaert correction. Best results were obtaining for the C-correction and the empiric–statistic correction. Decreases of the SD for bare soil pixels were larger than 100% for the C-correction and the empiric–statistic correction method compared to the other correction methods in the visible spectrum and larger than 50% in the IR region. In almost all tests the empiric–statistic method provided better results than the C-correction. When analyzing the multi-temporal stability, pixels under bad illumination conditions (northern orientation) improved after correction, while a deterioration was observed for pixels under good illumination conditions (southern orientation). Taken this observation into account, a simple but robust method for topographic correction of Landsat imagery is proposed. 相似文献
65.
66.
67.
首先利用海表面风速与高度的对数关系、风向与高度的关系,推算出高空的风速、风向及相应风力的大小。在此基础上根据降雨的形成高度,假定在海表面10 m处风速为10 m/s的情况下,得到单位质量为1的雨水在风场影响下的飘移距离在3—100 km之间,可以判定这个偏移距离即为在风场影响下卫星观测降雨的误差。利用上述方法对10组TRMM卫星降雨产品数据进行纠正,将纠正前后的TRMM数据与GPCP数据进行对比。结果显示,经过纠正的TRMM数据与GPCP数据更为一致,整体精度提高了12%左右,验证了方法的正确性。 相似文献
68.
69.
70.
手持GPS定位精度与误差的研究 总被引:2,自引:0,他引:2
分别探讨在绝对定位和相对定位两种模式下手持式GPS定位的稳定性,得出合理的观测时间长。通过不同时长的观测数据的对比分析给出:实时定位与长时间定位观测值之差在1m之内。手持GPS绝对定位的准确度即测量的结果与其真实位置符合程度非常高,能够控制在亚米级的范围之内。在卫星个数较多的情况下,实时定位的精度也能控制在亚米级的范围之内。利用单点定位系统误差改正模型,消除或减弱某些误差后能得到更高的精度,使得单点定位精度达到半米之内甚至更高。 相似文献