全文获取类型
收费全文 | 1715篇 |
免费 | 301篇 |
国内免费 | 321篇 |
专业分类
测绘学 | 103篇 |
大气科学 | 52篇 |
地球物理 | 759篇 |
地质学 | 937篇 |
海洋学 | 103篇 |
天文学 | 88篇 |
综合类 | 85篇 |
自然地理 | 210篇 |
出版年
2024年 | 7篇 |
2023年 | 23篇 |
2022年 | 65篇 |
2021年 | 53篇 |
2020年 | 63篇 |
2019年 | 83篇 |
2018年 | 68篇 |
2017年 | 66篇 |
2016年 | 64篇 |
2015年 | 85篇 |
2014年 | 82篇 |
2013年 | 99篇 |
2012年 | 100篇 |
2011年 | 122篇 |
2010年 | 82篇 |
2009年 | 112篇 |
2008年 | 89篇 |
2007年 | 112篇 |
2006年 | 135篇 |
2005年 | 111篇 |
2004年 | 102篇 |
2003年 | 82篇 |
2002年 | 65篇 |
2001年 | 81篇 |
2000年 | 46篇 |
1999年 | 58篇 |
1998年 | 45篇 |
1997年 | 57篇 |
1996年 | 43篇 |
1995年 | 44篇 |
1994年 | 23篇 |
1993年 | 16篇 |
1992年 | 11篇 |
1991年 | 8篇 |
1990年 | 9篇 |
1989年 | 6篇 |
1988年 | 9篇 |
1987年 | 2篇 |
1986年 | 5篇 |
1985年 | 1篇 |
1984年 | 1篇 |
1982年 | 1篇 |
1979年 | 1篇 |
排序方式: 共有2337条查询结果,搜索用时 15 毫秒
51.
It gradually becomes a common work using large seismic wave data to obtain source parameters, such as seismic moment, break radius, stress drop, with completingof digital seismic network in China (Hough, et al, 1999; Bindi, et al, 2001). These parameters are useful on earthquake prediction and seismic hazard analysis.Although the computation methods of source parameters are simple in principle and the many research works have been done, it is not easy to obtain the parameters accurately. There are two factors affecting the stability of computation results. The first one is the effect of spread path and site respond on signal. According to the research results, there are different geometrical spreading coefficients on different epicenter distance. The better method is to introduce trilinear geometrical spreading model (Atkinson, Mereu, 1992; Atkinson, Boore, 1995; WONG, et al, 2002). In addition, traditional site respond is estimated by comparing with rock station, such as linear inversion method (Andrews, 1982), but the comparative estimation will introduce some errors when selecting different stations. Some recent research results show that site respond is not flat for rock station (Moya, et al, 2000; ZHANG,. et al, 2001; JIN, et al, 2000; Dutta, et al, 2001). The second factor is to obtain low-frequency level and corner frequency fromdisplacement spectrum. Because the source spectrum model is nonlinear function,these values are obtained by eye. The subjectivity is strong. The small change of corner frequency will affect significantly the result of stress drop. 相似文献
52.
Jean-François Semblat Roberto Paolucci Anne-Marie Duval 《Comptes Rendus Geoscience》2003,335(4):365-370
For the analysis of seismic wave amplification, modal methods are interesting tools to study the modal properties of geological structures. Modal approaches mainly lead to information on such parameters as fundamental frequencies and eigenmodes of alluvial basins. For a specific alluvial deposit in Nice (France), a simplified modal approach involving the Rayleigh method is considered. This approach assumes a set of admissible shape functions for the eigenmodes and allows a fast estimation of the fundamental frequency of the basin. The agreement with other numerical results (Boundary Element Method) and experimental ones is fully satisfactory. The simplified modal method then appears as an efficient mean for the global vibratory characterization of geological structures towards resonance. To cite this article: J.-F. Semblat et al., C. R. Geoscience 335 (2003). 相似文献
53.
54.
A. Anagnostopoulos G. Koukis N. Sabatakakis G. Tsiambaos 《Geotechnical and Geological Engineering》2003,21(4):377-387
This study presents the results of Cone Penetration Tests (CPT) and estimated correlations with the results of other in-situ tests (standard penetration test, cross-hole, seismocone) and laboratory tests (classification and undrained shear strength tests). These tests cover nearly all types of penetrable soils in Greece and, together with the formulation of empirical correlations, complement and improve on previous studies due to the significant number of CPT measurements. 相似文献
55.
场地条件对地震动相干函数的影响 总被引:3,自引:1,他引:3
本通过弹性半空间内位错源的数值解法研究了曲岩地震动相干函数,采用有限元方法分析了一些典型场地的地表地震动相干函数,两的对比结果表明:复杂场地对地震动相干函数的影响强烈。 相似文献
56.
团树断层场地在多次地震中出现了烈度异常。为了弄清烈度异常的原因,应用显式有限元方法,数值模拟了在脉冲地震波斜入射情形下断层场地的地震反应。结果表明:在基岩山脚附近土层场地地震动放大比基岩山区平均高4倍、比远离基岩山脚土层场地平均高2倍,与历史震害分布有较好的对应。 相似文献
57.
介绍北京正负电子对撞机注和器复测的精度要求,阐述采用波带板激光准直系统与精密水准测量相结合的方法,进行注入器复测的观测、数据处理与调整。根据复测数据分析了隧道地基变形与加速管位置变形及其规律,提出了一些有益的结论与建议。 相似文献
58.
Ricardo J. Elia 《Natural Resources Research》1997,6(2):85-98
Archaeological sites, the material remnants of our human past, are finite and nonrenewable cultural resources that are under
constant threat from environmental forces, development activities, warfare, vandalism, and looting. Site looting is the destructive
removal of archaeological objects to supply the art market. Looting is part of an economic system, the antiquities market,
that works to supply the demand of collectors for archaeological objects. The destruction of archaeological resources by looters
is an international crisis and threatens to obliterate the world’s cultural heritage and our ability to understand past cultures.
The scale and intensity of the looting problem can be estimated by studying the extent of site destruction in countries of
origin and by investigating the sources of antiquities held by collectors. Finding a solution to the problem of looting will
require a focus on the demand side of the market (i.e., collectors) instead of the traditional focus on the supply side (looters,
dealers) 相似文献
59.
60.
The phase velocity and the attenuation coefficient of compressional seismic waves, propagating in poroelastic, fluid-saturated, laminated sediments, are computed analytically from first principles. The wavefield is found to be strongly affected by the medium heterogeneity. Impedance fluctuations lead to poroelastic scattering; variations of the layer compressibilities cause inter-layer flow (a 1-D macroscopic local flow). These effects result in significant attenuation and dispersion of the seismic wavefield, even in the surface seismic frequency range, 10–100 Hz. The various attenuation mechanisms are found to be approximately additive, dominated by inter-layer flow at very low frequencies. Elastic scattering is important over a broad frequency range from seismic to sonic frequencies. Biot's global flow (the relative displacement of solid frame and fluid) contributes mainly in the range of ultrasonic frequencies. From the seismic frequency range up to ultrasonic frequencies, attenuation due to heterogeneity is strongly enhanced compared to homogeneous Biot models. Simple analytical expressions for the P -wave phase velocity and attenuation coefficient are presented as functions of frequency and of statistical medium parameters (correlation lengths, variances). These results automatically include different asymptotic approximations, such as poroelastic Backus averaging in the quasi-static and the no-flow limits, geometrical optics, and intermediate frequency ranges. 相似文献