全文获取类型
收费全文 | 1601篇 |
免费 | 239篇 |
国内免费 | 344篇 |
专业分类
测绘学 | 91篇 |
大气科学 | 293篇 |
地球物理 | 395篇 |
地质学 | 759篇 |
海洋学 | 189篇 |
天文学 | 131篇 |
综合类 | 167篇 |
自然地理 | 159篇 |
出版年
2024年 | 10篇 |
2023年 | 27篇 |
2022年 | 83篇 |
2021年 | 87篇 |
2020年 | 61篇 |
2019年 | 99篇 |
2018年 | 70篇 |
2017年 | 83篇 |
2016年 | 89篇 |
2015年 | 59篇 |
2014年 | 96篇 |
2013年 | 70篇 |
2012年 | 74篇 |
2011年 | 73篇 |
2010年 | 97篇 |
2009年 | 96篇 |
2008年 | 94篇 |
2007年 | 81篇 |
2006年 | 58篇 |
2005年 | 65篇 |
2004年 | 25篇 |
2003年 | 43篇 |
2002年 | 37篇 |
2001年 | 41篇 |
2000年 | 71篇 |
1999年 | 80篇 |
1998年 | 55篇 |
1997年 | 44篇 |
1996年 | 57篇 |
1995年 | 45篇 |
1994年 | 43篇 |
1993年 | 34篇 |
1992年 | 23篇 |
1991年 | 20篇 |
1990年 | 16篇 |
1989年 | 24篇 |
1988年 | 16篇 |
1987年 | 7篇 |
1986年 | 6篇 |
1985年 | 4篇 |
1984年 | 2篇 |
1983年 | 5篇 |
1982年 | 5篇 |
1981年 | 1篇 |
1979年 | 3篇 |
1978年 | 1篇 |
1977年 | 2篇 |
1958年 | 2篇 |
排序方式: 共有2184条查询结果,搜索用时 616 毫秒
111.
四川彭县推覆构造的特征与形成 总被引:7,自引:0,他引:7
本文对前龙门山区彭县推覆构造进行了详细研究,在推覆体内部划分出若干不同的构造带,强烈压缩变形的白水河断裂带为其“根带”。它们主要是旱第三纪末的陆内俯冲挤压导致的褶皱-逆冲作用以及随后的重力滑动作用形成的。推覆体在滑移过程中发生变形,并对原地岩系的构造进行改造。 相似文献
112.
113.
随机地震模型及反应谱分析 总被引:2,自引:0,他引:2
本文以实际地震加速度的频谱特性和相位谱特性为依据,仿概率统计理论中的高斯概率密度函数,建立了随机地震加速度频数学模型。 相似文献
114.
40Ar/39Ar plateau ages of biotite, plagioclase, K-feldspar and hornblende from the Biluoxueshan and Lincang plutons in the three-river area of Yunnan and the Quxu pluton in the Gandise belt of Xizang indicate that the three plutons were emplaced at 420, 234 and 43.4 Ma, respectively. Based on the study of closure temperatures and thermal histories, it is shown that the Lincang and Biluoxueshan plutons experienced the same thermodynamic event during 85–90 Ma, temporally representing the collision between the Sundaland and Eurasian plates, and that the Quxu pluton was uplifted at a much faster rate during 40–44 Ma(2.6 mm/a), marking the collision between the Indian and Eurasian plates. 相似文献
115.
填充墙与钢框架协同工作性能非线性分析 总被引:5,自引:2,他引:5
在试验研究的基础上,运用ANSYS有限元中的接触单元建模,对加气混凝土填充墙钢框架的结构性能进行了研究,同时与纯钢框架结构在强度、刚度、以及延性等方面进行了对比分析,结果表明:填充墙与钢框架协同工作能够改善钢框架结构的受力性能和抗震能力,这为钢结构及其围护体系的研究与推广应用提供了一定的理论依据。 相似文献
116.
泾阳4.8级地震前后重力变化探析 总被引:2,自引:0,他引:2
系统分析了泾阳Ms4.8地震前后陕西关中地区流动重力观测资料,探讨了重力场的时空变化及其映震特征。结果表明:①震前在震中区附近形成较显著地重力负异常区,且与沉降区基本吻合。②泾阳地震震中区既是重力变化梯度带,也是重力异常的正值区到负值区的过度带。③由于震源区应力作用方式是以水平为主的左旋走滑运动,震前局部重力异常不显著。 相似文献
117.
利用成熟的、性能优异的GMT和SAC作为后台处理软件,并辅以MySQL数据库系统来管理数据。实现了地震快速数据的自动、及时发布。 相似文献
118.
Common‐conversion‐point binning associated with converted‐wave (C‐wave) processing complicates the task of parameter estimation, especially in anisotropic media. To overcome this problem, we derive new expressions for converted‐wave prestack time migration (PSTM) in anisotropic media and illustrate their applications using both 2D and 3D data examples. The converted‐wave kinematic response in inhomogeneous media with vertical transverse isotropy is separated into two parts: the response in horizontally layered vertical transverse isotrophy media and the response from a point‐scatterer. The former controls the stacking process and the latter controls the process of PSTM. The C‐wave traveltime in horizontally layered vertical transverse isotrophy media is determined by four parameters: the C‐wave stacking velocity VC2, the vertical and effective velocity ratios γ0 and γeff, and the C‐wave anisotropic parameter χeff. These four parameters are referred to as the C‐wave stacking velocity model. In contrast, the C‐wave diffraction time from a point‐scatterer is determined by five parameters: γ0, VP2, VS2, ηeff and ζeff, where ηeff and ζeff are, respectively, the P‐ and S‐wave anisotropic parameters, and VP2 and VS2 are the corresponding stacking velocities. VP2, VS2, ηeff and ζeff are referred to as the C‐wave PSTM velocity model. There is a one‐to‐one analytical link between the stacking velocity model and the PSTM velocity model. There is also a simple analytical link between the C‐wave stacking velocities VC2 and the migration velocity VCmig, which is in turn linked to VP2 and VS2. Based on the above, we have developed an interactive processing scheme to build the stacking and PSTM velocity models and to perform 2D and 3D C‐wave anisotropic PSTM. Real data applications show that the PSTM scheme substantially improves the quality of C‐wave imaging compared with the dip‐moveout scheme, and these improvements have been confirmed by drilling. 相似文献
119.
A novel method of synthesizing seismic wave using wavelet reconstruction is proposed and compared with the traditional method of using theory of Fourier transform. By adjusting the frequency band energy and taking it as criterion, the formula of synthesizing seismic wave is deduced. Using the design parameters specified in Chinese Seismic Design Code for buildings, seismic waves are synthesized. Moreover, the method of selecting wavelet bases in synthesizing seismic wave and the influence of the damping ratio on synthesizing results are analyzed. The results show that the synthesis seismic waves using wavelet bases can represent the characteristics of the seismic wave as well as the ground characteristic period, and have good time-frequency non-stationary. 相似文献
120.
The No. 6 Coal-bed from the Heidaigou Mine, Jungar Coalfield, Inner Mongolia is a super-large Ga deposit. The dominant carrier of Ga is boehmite in coal. The study of coal facies may provide genetic enrichment information of Ga and its carrier (boehmite) in the Ga deposit. On the basis of study on coal petrology and mineralogy, it was found that the No. 6 Coal-bed from the Heidaigou Mine of Jungar was enriched in inertinites and the microlitho-types were dominated by clarodurite. The maceral morphological features and association indicate that the coal-bed was formed in a dry sedimentary environment or in a periodic dry sedimentary environment caused by the alternating variations of groundwater level. The optimum conditions for the enrichment of Ga and its particular carrier (boehmite) were dominated by four transitional conditions: (1) the upper delta plain which was the transitional zone between alluvial and lower delta plains, (2) the transitional zone between the dry and wet forest swamps, being slightly apt to the dry one, (3) the transitional tree density between the thick and loose ones, and (4) the low moor that was the transitional zone between two high moors during peat accumulation. 相似文献