全文获取类型
收费全文 | 4569篇 |
免费 | 915篇 |
国内免费 | 1279篇 |
专业分类
测绘学 | 307篇 |
大气科学 | 806篇 |
地球物理 | 1171篇 |
地质学 | 2224篇 |
海洋学 | 938篇 |
天文学 | 238篇 |
综合类 | 598篇 |
自然地理 | 481篇 |
出版年
2024年 | 47篇 |
2023年 | 108篇 |
2022年 | 222篇 |
2021年 | 256篇 |
2020年 | 238篇 |
2019年 | 255篇 |
2018年 | 315篇 |
2017年 | 277篇 |
2016年 | 295篇 |
2015年 | 220篇 |
2014年 | 277篇 |
2013年 | 262篇 |
2012年 | 354篇 |
2011年 | 312篇 |
2010年 | 299篇 |
2009年 | 279篇 |
2008年 | 226篇 |
2007年 | 253篇 |
2006年 | 206篇 |
2005年 | 190篇 |
2004年 | 131篇 |
2003年 | 127篇 |
2002年 | 97篇 |
2001年 | 111篇 |
2000年 | 157篇 |
1999年 | 213篇 |
1998年 | 146篇 |
1997年 | 169篇 |
1996年 | 119篇 |
1995年 | 109篇 |
1994年 | 102篇 |
1993年 | 99篇 |
1992年 | 68篇 |
1991年 | 53篇 |
1990年 | 45篇 |
1989年 | 30篇 |
1988年 | 20篇 |
1987年 | 19篇 |
1986年 | 8篇 |
1985年 | 6篇 |
1984年 | 6篇 |
1983年 | 12篇 |
1982年 | 6篇 |
1981年 | 7篇 |
1980年 | 2篇 |
1979年 | 3篇 |
1977年 | 1篇 |
1958年 | 2篇 |
1957年 | 1篇 |
1954年 | 2篇 |
排序方式: 共有6763条查询结果,搜索用时 15 毫秒
121.
Introduction Based on the elastic theory of the hard inclusion (Dobrovolskii, 1991), we developed an inclusion theory of rheologic medium, and applied the results of bulk-strain field of a rheologic inclusion model to explain the spatial-temporal evolution process of earthquake precursors (SONG, et al, 2000). In the former paper (SONG, et al, 2003), we derived the viscoelastic displacement field of the rheologic inclusion model on the basis of the analytic expression of displacement field o… 相似文献
122.
Seepage driving effect on deformations of San Fernando dams 总被引:2,自引:0,他引:2
In the process of flow deformation of an earth dam, the seepage force inside the dam plays a role as a driving force. The seepage force acts just like the gravitational force in terms of pushing soils away from their original locations after liquefaction is triggered. This paper draws attention to this seepage driving effect by presenting a set of fully coupled finite element analyses on the well-known San Fernando dams, with the objective of evaluating the impact of this seepage effect. The results indicate that while this effect is always there, its practical significance depends on a number of factors. In the case of the upper San Fernando dam, which experienced a significant, but restricted, downstream movement during the 1971 earthquake, the seepage driving effect was indeed significant. On the contrary, for the lower dam, which failed and slid into the upstream reservoir during the same earthquake, this seepage effect was relatively less pronounced. The detailed results of the analyses reveal the likely mechanisms of failure and deformation of the two dams and the likely cause behind the difference between their responses during the earthquake. 相似文献
123.
Cross-sensor calibration between Ikonos and Landsat ETM+ for spectral mixture analysis 总被引:1,自引:0,他引:1
Conghe Song 《Geoscience and Remote Sensing Letters, IEEE》2004,1(4):272-276
Spectral mixture analysis is an algorithm that is developed to overcome the weakness in traditional land-use/land-cover (LULC) classification where each picture element (pixel) from remote sensing is assigned to one and only one LULC type. In reality, a remotely sensed signal from a pixel is often a spectral mixture from several LULC types. Spectral mixture analysis can derive subpixel proportions for the endmembers from remotely sensed data. However, one frequently faces the problem in determining the spectral signatures for the endmembers. This study provides a cross-sensor calibration algorithm that enables us to obtain the endmember signatures from an Ikonos multispectral image for spectral mixture analysis using Landsat ETM+ images. The calibration algorithm first converts the raw digital numbers from both sensors into at-satellite reflectance. Then, the Ikonos at-satellite reflectance image is degraded to match the spatial resolution of the Landsat ETM+ image. The histograms at the same spatial resolution from the two images are matched, and the signatures from the pure pixels in the Ikonos image are used as the endmember signatures. Validation of the spectral mixture analysis indicates that the simple algorithm works effectively. The algorithm is not limited to Ikonos and Landsat sensors. It is, in general, applicable to spectral mixture analysis where a high spatial resolution sensor and a low spatial resolution sensor with similar spectral resolutions are available as long as images collected by the two sensors are close in time over the same place. 相似文献
124.
125.
Determination of the elastic modulus set of foliated rocks from ultrasonic velocity measurements 总被引:2,自引:0,他引:2
Ultrasonic measurements of compressional and shear wave velocities under hydrostatic pressure up to 70 MPa were carried out on cylindrical specimens cored across and along the foliation planes. Our measurements revealed that the foliation of the metamorphic rocks induces a clear velocity anisotropy between two orthogonal directions; faster along the foliation plane and slower across the plane in most rock types. All velocity components monotonically increase with the confining pressure, probably due to the closure of microcracks distributed in rock specimens. We determined the complete set of dynamic moduli of foliated metamorphic rocks with two assumptions; transverse isotropy due to the foliation and ellipsoidal seismic energy propagation from a point source. The calculated elastic moduli referring to different directions could be valuable for the design of various engineering structures in planar textured rock mass. 相似文献
126.
We investigate the thermo-mechanical properties beneath the young orogenic belt of Taiwan by constructing a shear strength profile from a vertical stratified rheological structure. The stratified rheological structure is estimated based on the recently developed thermal structure and its likely composition. Subduction–collision in the young orogenic belts and the thick accretionary wedge make a significant contribution to the growth of sialic crust in the hinterland. The sialic bulk crust not only results in a low seismic velocity but also produces weak crust in the hinterland. The earthquake depth–frequency distribution in the foreland and hinterland correlates very well with the regimes of the brittle/ductile transition revealed in the strength profile. Our results show that the observed two-layer seismicity in the foreland is due to a moderate geotherm and an intermediate mafic bulk composition; while single-layer seismicity in the hinterland is due to its felsic bulk composition. In the foreland, the mechanically strong crust (MSC) and the mechanically strong lithosphere (MSL) coincide with frequent seismicity. The shallow MSC in the hinterland is consistent with the 20- to 25-km seismicity occurring there. The total lithospheric integrated strength (LIS) in the hinterland is only about half of that in the foreland, suggesting a weak lower crust and lithosphere mantle in the hinterland. The results confirm that the earthquake cutoff depth is a proxy for temperature. The calculated decrease of effective elastic thickness (EET) from the orogenic margin (foreland) to the center (hinterland) is consistent with the results of flexure modeling in most orogenic belts. Due to the weak LIS in the hinterland, crustal thinning and rifting may occur in the future. Our results, thus, suggest that the mechanical structure is also closely related to the composition and is not directly reflected in the thermal structure. 相似文献
127.
128.
129.
从怀来4井水化学异常变化分析流体在孕震过程中的作用 总被引:1,自引:0,他引:1
20世纪60年代,流体在地震孕育与发生过程中的作用就已受到研究者关注。如Evans(1966)发现美国洛基山兵工厂周围地震活动与深井注入废液有关。在我国的地壳流体活动与诱发地震关系的研究方面,也取得了很多成果。针对上地壳流体与地震活动的关系,前人在辽东半岛、东南沿海、红河断裂带、京津地区进行了系统研究。结果表明,地壳热流体活动区的地震活动多,但多为中小地震;而地壳热流体活动弱的地区地震活动数量相对少,但以大震活动为主。近年来,地下流体在孕震过程与构造活动中的作用的研究已有了一些进展。 相似文献
130.