全文获取类型
收费全文 | 18717篇 |
免费 | 4332篇 |
国内免费 | 4844篇 |
专业分类
测绘学 | 858篇 |
大气科学 | 1249篇 |
地球物理 | 8749篇 |
地质学 | 11990篇 |
海洋学 | 1969篇 |
天文学 | 512篇 |
综合类 | 1214篇 |
自然地理 | 1352篇 |
出版年
2024年 | 75篇 |
2023年 | 222篇 |
2022年 | 518篇 |
2021年 | 588篇 |
2020年 | 651篇 |
2019年 | 881篇 |
2018年 | 701篇 |
2017年 | 730篇 |
2016年 | 822篇 |
2015年 | 944篇 |
2014年 | 1122篇 |
2013年 | 1178篇 |
2012年 | 1182篇 |
2011年 | 1265篇 |
2010年 | 1047篇 |
2009年 | 1284篇 |
2008年 | 1259篇 |
2007年 | 1328篇 |
2006年 | 1339篇 |
2005年 | 1094篇 |
2004年 | 1082篇 |
2003年 | 945篇 |
2002年 | 835篇 |
2001年 | 744篇 |
2000年 | 820篇 |
1999年 | 761篇 |
1998年 | 706篇 |
1997年 | 636篇 |
1996年 | 595篇 |
1995年 | 536篇 |
1994年 | 422篇 |
1993年 | 371篇 |
1992年 | 286篇 |
1991年 | 199篇 |
1990年 | 184篇 |
1989年 | 145篇 |
1988年 | 128篇 |
1987年 | 71篇 |
1986年 | 33篇 |
1985年 | 23篇 |
1984年 | 35篇 |
1983年 | 8篇 |
1982年 | 9篇 |
1981年 | 6篇 |
1980年 | 8篇 |
1979年 | 22篇 |
1978年 | 14篇 |
1977年 | 21篇 |
1954年 | 18篇 |
排序方式: 共有10000条查询结果,搜索用时 328 毫秒
291.
准噶尔盆地基底火山岩中的辉石及其对盆地基底性质的示踪 总被引:4,自引:0,他引:4
根据钻井和航磁资料,准噶尔盆地基底可划分为西、北、南三区。3个地区火山岩中辉石的化学成分、种属名称各不相同。辉石化学成分反映出来的寄主岩的碱度、碱度演化趋势以及寄主岩形成的构造环境、构造环境演化史均各有差异,佐证了准噶尔盆地基底是由哈萨克斯坦板块东南缘、西伯利亚板块西南缘和塔里木板块北缘增生大陆拼合而成。其中西、北两区拼合较早,早石炭世末的早海西运动时抬升成陆;南区成陆较晚,晚古炭世末的晚海西运动使南区与西、北两区联合大陆对接,形成完整的准噶尔盆地海西褶皱基底。 相似文献
292.
气藏评价尚未结束之前,开发的早期部署工作非常困难。针对洛带气田蓬莱镇组气藏的开发部署工作,利用目前许多新方法对开发层系划分、采气规模、开发规划、合理配产和井网部署等进行了优化研究,对气藏开发提出了指导性意见,且对类似气藏也具有参考意义。 相似文献
293.
Apatite fission track analysis was performed on 56 samples from central Spain to unravel the far field effects of the Alpine plate tectonic history of Iberia. The modelled thermal histories reveal complex cooling in the Cenozoic, indicative of intermittent denudation. Accelerated cooling events occurred across the Spanish Central System (SCS) from the Middle Eocene to Recent. These accelerated cooling events resulted in up to 2.8±0.9 km of denudation in the western Sierra de Gredos and 3.6±1.0 km in the central and eastern Gredos (assuming a paleogeothermal gradient of 28±5 °C and a surface temperature of 10 °C). The greatest amount of denudation (5.0±1.6 km) occurred in the Sierra de Guadarrama. Accompanying rock uplift was 4.7±1.0 and 5.9±1.6 km in the eastern Gredos and Guadarrama, respectively. Most denudation in the Gredos occurred from the Middle Eocene to the Early Miocene and can be related to the N–S stress field, induced by the Pyrenean compression. In the Guadarrama, the greatest denudation was Pliocene to Recent of age and seems related to the ongoing NW–SE Betic compression. The fact that the formation of the E–W trending Gredos coincides with the N–S Pyrenean compression and the creation of the present day morphology of the NE–SW trending Guadarrama with the younger NW–SE Betic compression, indicates that they record the far field effects of Alpine plate tectonics on Iberia. The trend of pre-existing lineaments was of major importance in influencing the style and magnitude of these of far field effects. 相似文献
294.
A major earthquake (M=6.6) occurred on 21 June 2000, in South Iceland. This paper presents an unusual example of left-lateral strike-slip displacement recorded in a newly asphalted car park surface through a mechanically consistent pattern of open fissures and pressure ridges resulting from simple shear and rotation. Measurement of these features allows accurate reconstruction of the local deformation. The behaviour of the asphalt layer resembles that of analogue physical models, especially in terms of rotations induced by shear deformation. It is finally shown that through a wide range of scales some basic patterns associating rotation and opposite senses of strike-slip exist in the South Iceland Seismic Zone. 相似文献
295.
Ground fissuring is a recurrent problem in many countries where water extraction surpasses the natural recharge of aquifers. Due to differential settlement, the soil layer undergoes deformation and cracks with serious consequences for civil infrastructure. Here, we propose an approximate analysis of the fissuring process that can be used to predict the location of cracks, which increasingly affect some middle- and large-sized cities in the world. For that purpose, the ground loss theory is applied to sediments overlying a sinusoidal-shaped graben. This analysis shows the existence of a tensile zone at the border of the graben with maximal values on its shoulder where tension cracks are more likely to appear. It also shows that soil deformation under differential settlement may evolve into ground faulting if water withdrawal continues. Finally, when a crack has completely developed, the tensile zone shifts towards the center of the graben, creating a new area for potential cracking and faulting. 相似文献
296.
Crack damage stress as a composite function of porosity and elastic matrix stiffness in dolomites and limestones 总被引:4,自引:0,他引:4
Twenty-five uniaxial compression tests were performed to determine stress at onset of dilation, referred to herein as “the crack damage stress,” in heterogeneous dolomites and limestones. A simplified model for crack damage stress (σcd) is developed here using porosity, elastic modulus, Poisson's ratio and three empirical coefficients. The model shows that when porosity decreases and elastic modulus increases, σcd rapidly increases and approaches its maximum value. On the other hand, when porosity increases and elastic modulus decreases, σcd rapidly decreases and approaches its minimum value. The proposed model is validated for six heterogeneous limestone and dolomite formations which are widely distributed in Israel. 相似文献
297.
298.
Amal Saidi Abdelfatah Tahiri Lahcen Ait Brahim Maraim Saidi 《Comptes Rendus Geoscience》2002,334(3):221-226
The fracturing analysis in the Permian basins of Jebilet and Rehamna (Hercynian Morocco) and the underlying terranes allowed us to suggest a model for their opening. Three tectonic episodes are distinguished: a transtensional episode NNE–SSW-trending (Permian I), occurring during the opening along sinistral wrench faults N70–110-trending, associated with synsedimentary normal faults; a transpressive episode ESE–WNW-trending (Permian II), initiating the closure, the normal faults playing back reverse faults and the N70 trending faults dextral wrench faults; a compressional episode NNW–SSE (post-Permian, ante-Triassic), accentuating the closure and the deformation and putting an end to the Tardi-Hercynian compressive movements. To cite this article: A. Saidi et al., C. R. Geoscience 334 (2002) 221–226. 相似文献
299.
300.