全文获取类型
收费全文 | 7003篇 |
免费 | 1469篇 |
国内免费 | 2393篇 |
专业分类
测绘学 | 92篇 |
大气科学 | 342篇 |
地球物理 | 1218篇 |
地质学 | 7756篇 |
海洋学 | 478篇 |
天文学 | 11篇 |
综合类 | 304篇 |
自然地理 | 664篇 |
出版年
2024年 | 57篇 |
2023年 | 127篇 |
2022年 | 225篇 |
2021年 | 277篇 |
2020年 | 311篇 |
2019年 | 313篇 |
2018年 | 290篇 |
2017年 | 329篇 |
2016年 | 370篇 |
2015年 | 335篇 |
2014年 | 423篇 |
2013年 | 532篇 |
2012年 | 494篇 |
2011年 | 547篇 |
2010年 | 414篇 |
2009年 | 515篇 |
2008年 | 502篇 |
2007年 | 511篇 |
2006年 | 564篇 |
2005年 | 429篇 |
2004年 | 431篇 |
2003年 | 373篇 |
2002年 | 369篇 |
2001年 | 324篇 |
2000年 | 359篇 |
1999年 | 274篇 |
1998年 | 203篇 |
1997年 | 223篇 |
1996年 | 180篇 |
1995年 | 152篇 |
1994年 | 111篇 |
1993年 | 77篇 |
1992年 | 64篇 |
1991年 | 39篇 |
1990年 | 32篇 |
1989年 | 25篇 |
1988年 | 27篇 |
1987年 | 13篇 |
1986年 | 9篇 |
1985年 | 2篇 |
1984年 | 1篇 |
1983年 | 2篇 |
1982年 | 2篇 |
1981年 | 1篇 |
1980年 | 1篇 |
1978年 | 3篇 |
1977年 | 1篇 |
1976年 | 1篇 |
1954年 | 1篇 |
排序方式: 共有10000条查询结果,搜索用时 31 毫秒
221.
222.
Dominique Dumas 《Comptes Rendus Geoscience》2004,336(13):1149-1159
This study seeks to determine suspended-matter flux of the Isère at Grenoble, one of the most important rivers of the northern French Alps. Since 1994, and especially 1996, systematic samplings of the left bank make it possible to follow in one point the variations of suspended particles and matter (SPM) of this river. But from a single measurement, sometimes not very representative of the whole observable concentrations within the section, it remains still difficult to estimate precisely the SPM flux. The results of this study show in particular the successive appearance of several turbidity gradients, whose occurrence is explained mainly by the hydrological and hydro-sedimentary dynamics of this river. The estimate of these gradients thus makes it possible to extrapolate specific measurements more easily and consequently to daily define the quantities of suspended matter exported by the Isère. Since 1996, the results show a very high flow, specific of the Isère at Grenoble, variable between 124 and more than 460 t km?2 yr?1. To cite this article: D. Dumas, C. R. Geoscience 336 (2004). 相似文献
223.
Alik Ismail-Zadeh Igor Tsepelev Chistopher Talbot Alexander Korotkii 《Tectonophysics》2004,387(1-4):81-103
Numerical studies of ductile deformations induced by salt movements have, until now, been restricted to two-dimensional (2D) modelling of diapirism. This paper suggests a numerical approach to model the evolution of three-dimensional (3D) salt structures toward increasing maturity. This approach is also used here to restore the evolution of salt structures through successive earlier stages. The numerical methodology is applied to study several model examples. We analyse a model of salt diapirs that develop from an initial random perturbation of the interface between salt and its overburden and restore the evolved salt diapirs to their initial stages. We show that the average restoration errors are less than 1%. An evolutionary model of a 2D salt wall loaded by a 2D pile of sediments predicts a decomposition of the salt wall into 3D diapiric structures when the overburden of salt is supplied by 3D synkinematic wedge of sediments. We model salt extrusion feeding a gravity current over the depositional surface and estimate an average rate of extrusion and horizontal velocity of salt spreading. Faulting of the overburden to salt overhangs initiates new secondary diapirs, and we analyse the growth of these secondary diapirs. We also study how lateral flow effects the evolution of salt diapirs. The shape of a salt diapir can be very different if the rate of horizontal flow is much greater than the initial rate of diapiric growth solely due to gravity. We discuss the applicability of the results of the models to the evolution of Late Permian salt structures in the Pricaspian basin (Russia and Kazakhstan). These structures are distinguishable into a variety of styles representing different stages of growth: salt pillows, diapirs, giant salt massifs, 2D diapiric walls and 3D stocks complicated by large overhangs. The different sizes, shapes and maturities of salt structures in different parts of the Pricaspian basin reflect areal differences in salt thickness and loading history. Our results suggest that the numerical methodology can be employed to analyse the evolution of all salt structures that have upbuilt through younger ductile overburdens. 相似文献
224.
Zoltn Hajnal Endre Hegeds G. Randy Keller Tams Fancsik Attila Cs. Kovcs Rbert Csabafi 《Tectonophysics》2004,388(1-4):239
A specially designed 700-km2 grid survey, deploying 1000 regularly distributed low-frequency seismic recording systems, successfully investigated one of the most complex geologic environments of the Pannonian basin. The wide-angle signals penetrated through over 1000 m of multi-phase igneous lithology and recognized, for the first time, the underlying enigmatic Permian to Early Triassic basement rocks. Tomographic inversion of the first arrival grid data resulted in determination of an accurate three-dimensional (3-D) velocity field, to a depth of 4 km. The anomalous changes of the spatial velocity data outline the regional extent of the Late Miocene magmatic intrusions, which are covered by over 2000 m of Mid-Miocene to Pleistocene clastics. Complex relationship was found between the surface potential data and the intrusive bodies. This multi-faceted geophysical data analysis established a functional technique for mapping a subsurface with intricate acoustic and structural complexity. 相似文献
225.
226.
四川盆地潜在震源区的细致划分 总被引:2,自引:0,他引:2
四川盆地包括川中台拱和川东陷褶束的范围,具有相对稳定的大地构造环境.鉴于该地区地震活动水平相对较低、发震构造不甚明确的特点,在编制1990年版中国地震烈度区划图时,划分的潜在震源区面积也相对较大.本文在总结四川盆地中强地震(Ms=4.7-5.7)发震构造条件的基础上,用地震构造类比原则对四川盆地的潜在震源区进行了重新划分.确定潜在震源区边界时,充分考虑了背斜轴走向、背斜构造的影响带宽度、小震活动密集条带和余震的分布范围.得到了四川盆地更加细致的潜在震源区划分方案.这对于低地震活动水平地区的潜在震源区的细化研究具有一定参考意义。 相似文献
227.
山西临汾盆地近期地震活动性分析 总被引:1,自引:0,他引:1
通过对临汾盆地内近期地震活动频度和地震活动图像的分析,认为未来中强地震最有可能发生在近期地震活动较稀少的地段,能量积累的优势层位为5km~15km。 相似文献
228.
山西大同-阳高地震活动背景 总被引:2,自引:1,他引:2
通过对大同盆地历史地震活动及大同盆地历史地震活动与华北地震区、山西地震带强震活动的关系的研究,得出山西大同-阳高1989年6.1级地震活动是这一地区历史地震的延续,是华北北部中强地震活动的重要组成部分,具有广义前震的重要意义,其后对应发生的河北张北6.2级地震。标志着华北地震区的地震活动期已进入尾声。 相似文献
229.
230.