全文获取类型
收费全文 | 1376篇 |
免费 | 221篇 |
国内免费 | 627篇 |
专业分类
测绘学 | 27篇 |
大气科学 | 23篇 |
地球物理 | 479篇 |
地质学 | 1419篇 |
海洋学 | 70篇 |
天文学 | 4篇 |
综合类 | 31篇 |
自然地理 | 171篇 |
出版年
2024年 | 5篇 |
2023年 | 10篇 |
2022年 | 31篇 |
2021年 | 31篇 |
2020年 | 44篇 |
2019年 | 75篇 |
2018年 | 73篇 |
2017年 | 59篇 |
2016年 | 72篇 |
2015年 | 96篇 |
2014年 | 86篇 |
2013年 | 148篇 |
2012年 | 96篇 |
2011年 | 122篇 |
2010年 | 101篇 |
2009年 | 128篇 |
2008年 | 109篇 |
2007年 | 103篇 |
2006年 | 105篇 |
2005年 | 101篇 |
2004年 | 122篇 |
2003年 | 67篇 |
2002年 | 51篇 |
2001年 | 59篇 |
2000年 | 38篇 |
1999年 | 47篇 |
1998年 | 42篇 |
1997年 | 39篇 |
1996年 | 35篇 |
1995年 | 28篇 |
1994年 | 19篇 |
1993年 | 16篇 |
1992年 | 7篇 |
1991年 | 10篇 |
1990年 | 7篇 |
1989年 | 3篇 |
1988年 | 8篇 |
1987年 | 7篇 |
1986年 | 9篇 |
1985年 | 1篇 |
1984年 | 4篇 |
1983年 | 3篇 |
1982年 | 3篇 |
1981年 | 2篇 |
1978年 | 1篇 |
1974年 | 1篇 |
排序方式: 共有2224条查询结果,搜索用时 296 毫秒
41.
42.
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
43.
Reflection and transmission of seismic waves at an interface betwen two saturated soils 总被引:2,自引:0,他引:2
ReflectionandtransmisionofseismicwavesataninterfacebetwentwosaturatedsoilsJUNYANG(杨峻)SHIMINGWU(吴世明)ZhejiangUniversity,Hangz... 相似文献
44.
饱和土地基在既有房屋长期荷载作用下,地基土强度参数值随着地基土的排水固结和压密而提高,地基极限承载力也同时增大,如何估算此提高值而挖掘其潜力,传统方法只是借助于统计回归讨论了设计承载力。本文从土力学基本原理出发,借助Prandtl假定,对既有房屋饱和土地基极限承载力的增长进行了探讨。 相似文献
45.
我国特殊岩土研究 总被引:1,自引:0,他引:1
顾宝和 《水文地质工程地质》1997,24(2):43-45
本文分析,总结了我国特殊岩土理论与应用研究方面的新进展,内容涉及湿陷性黄土,软土膨胀岩土,红土,软岩和特殊土的结构性,指出需要进一步研究的问题,最后对特殊土的研究方法做了阐述。 相似文献
46.
雷州半岛英峰岭剖面多期红土矿物学特征初步研究 总被引:3,自引:0,他引:3
雷州半岛英峰岭剖面多期红土矿物学特征初步研究*文国高文启忠朱照宇徐义芳(中国科学院广州地球化学研究所,广州510640)关键词多期红土矿物学红土化雷州半岛我国南方热带-亚热带广泛发育的红土(包括红色风化壳和红色古土壤),记录了形成过程环境变迁的重要信... 相似文献
47.
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
48.
P-SH conversion is commonly observed in teleseismic P waves, and is often attributed to dipping interfaces beneath the receiver. Our modelling suggests an alternative explanation in terms of flat-layered anisotropy. We use reflectivity techniques to compute three-component synthetic seismograms in a 1-D anisotropic layered medium. For each layer of the medium, we prescribe values of seismic velocities and hexagonally symmetric anisotropy about a common symmetry axis of arbitrary orientation. A compressional wave in an anisotropic velocity structure suffers conversion to both SV -and SH -polarized shear waves, unless the axis of symmetry is everywhere vertical or the wave travels parallel to all symmetry axes. The P-SV conversion forms the basis of the widely used 'receiver function' technique. The P-SH conversion occurs at interfaces where one or both layers are anisotropic. A tilted axis of symmetry and a dipping interface in isotropic media produce similar amplitudes of both direct ( P ) and converted ( Ps ) phases, leaving the backazimuth variation of the P-Ps delay as the main discriminant. Seismic anisotropy with a tilted symmetry axis leads to complex synthetic seismograms in velocity models composed of just a few flat homogeneous layers. It is possible therefore to model observations of P coda with prominent transverse components with relatively simple 1-D velocity structures. Successful retrieval of salient model characteristics appears possible using multiple realizations of a genetic-algorithm (GA) inversion of P coda from several backazimuths. Using GA inversion, we determine that six P coda recorded at station ARU in central Russia are consistent with models that possess strong (> 10 per cent) anisotropy in the top 5 km and between 30 and 43 km depth. The symmetry axes are tilted, and appear aligned with the seismic anisotropy orientation in the mantle under ARU suggested by SKS splitting. 相似文献
49.
膨胀土判别与分类的灰关联分析法 总被引:13,自引:3,他引:13
基于灰色系统理论,给出一种用于膨胀土判别与分类的新方法—灰关联分析法。实际算例表明,该法具有简单方便、结果客观可靠等优点。 相似文献
50.