全文获取类型
收费全文 | 3876篇 |
免费 | 397篇 |
国内免费 | 487篇 |
专业分类
测绘学 | 1380篇 |
大气科学 | 588篇 |
地球物理 | 641篇 |
地质学 | 622篇 |
海洋学 | 276篇 |
天文学 | 636篇 |
综合类 | 388篇 |
自然地理 | 229篇 |
出版年
2024年 | 10篇 |
2023年 | 24篇 |
2022年 | 57篇 |
2021年 | 84篇 |
2020年 | 108篇 |
2019年 | 141篇 |
2018年 | 83篇 |
2017年 | 144篇 |
2016年 | 157篇 |
2015年 | 178篇 |
2014年 | 186篇 |
2013年 | 262篇 |
2012年 | 209篇 |
2011年 | 242篇 |
2010年 | 183篇 |
2009年 | 227篇 |
2008年 | 225篇 |
2007年 | 293篇 |
2006年 | 255篇 |
2005年 | 202篇 |
2004年 | 177篇 |
2003年 | 154篇 |
2002年 | 152篇 |
2001年 | 123篇 |
2000年 | 112篇 |
1999年 | 96篇 |
1998年 | 127篇 |
1997年 | 95篇 |
1996年 | 73篇 |
1995年 | 70篇 |
1994年 | 59篇 |
1993年 | 50篇 |
1992年 | 43篇 |
1991年 | 25篇 |
1990年 | 30篇 |
1989年 | 26篇 |
1988年 | 27篇 |
1987年 | 20篇 |
1986年 | 12篇 |
1985年 | 6篇 |
1984年 | 6篇 |
1982年 | 3篇 |
1981年 | 2篇 |
1980年 | 1篇 |
1954年 | 1篇 |
排序方式: 共有4760条查询结果,搜索用时 31 毫秒
61.
These last 10 years, numerical models of mantle convection have emphasized the role of the 670 km endothermic phase change in generating avalanches that trigger catastrophic mass transfers between upper and lower mantle. On the other hand, scientists have emphasized the concomitance of large-scale worldwide geophysical and tectonic events, which could find their deep thermal roots in the huge mass transfers induced by the avalanches. In particular, the paleontological records show two periods of length of day (l.o.d.) shortening between 420 and 360, and 200 and 80 Myr BP. This last event is synchronous with a strong true polar wander and a global warming of the upper mantle. In order to study the potential effects of the avalanche on the main component of the Earth’s rotation, the Liouville equation has been solved and the l.o.d. evolution has been calculated from the perturbations of the inertia tensor. The results show that the inertia tensor of the Earth’s is mainly sensitive to the global transfers through the 670 km discontinuity. The l.o.d. perturbations will be synchronous with the global thermal effects of the avalanche. These theoretical results allow proposing a self-consistent physical mechanism to explain periods of the Earth’s rotation acceleration. Within this context, the l.o.d. shortening during the Cenozoic and Cretaceous brings one more clue to the possible participation of a mantle avalanche in generating the concomitant large scale events which have occurred during this very particular period of the Earth’s history. 相似文献
62.
E. Schill C. CrouzetP. Gautam V.K. SinghE. Appel 《Earth and Planetary Science Letters》2002,203(1):45-57
In metacarbonates of the Lesser (LH) and Tethyan (TH) Himalayas of Kumaon/Garhwal (N-India) characteristic remanent magnetisations carried by pyrrhotite (unblocking temperatures: 250-330°C) and magnetite (demagnetising spectra: 15-50 mT) have been identified. Negative fold tests indicate remanence acquisition after the main folding phase, which is of short-wavelength character and occurs during the early orogenese of the Himalayas. A thermal or thermochemical origin of magnetisation is likely and the age of remanence acquisition is indicated to be about 40 Ma by 40K/39Ar cooling and 40Ar/39Ar crystallisation ages. In the Kumaon LH a long-wavelength tilting is indicated by a distribution of the remanence directions along a small-circle in N-S direction. Steepening of the remanence directions in the TH related to ramping on the Main Central Thrust (MCT) was not observed, in contrast to other related studies. In the Alaknanda valley of LH a 38±8 Ma age of remanence acquisition is supported by comparison of observed inclinations to the apparent polar wander path of India. Clockwise rotation of 20.3±11.7° (LH/Alaknanda valley) and 11.3±8.5° (TH) with respect to the Indian plate is observed, indicating that there is no significant evidence for rotational shortening along the MCT since about 40 Ma. Our results suggest that most of rotational underthrusting and oroclinal bending has not been accommodated by the MCT, but by the main thrusts south of it. The latest Miocene/Pliocene age of the Main Boundary Thrust indicates that oroclinal bending is a late-orogenic process. 相似文献
63.
JIANG Guorong ZHANG Ren SHA Wenyu YAN Junyue YAO Huadong 《Acta Meteorologica Sinica》2002,16(1):123-132
In the context of tower measured radiation datasets.following the correction principle meeting a diagnostic equation in data quality control and in terms of a technique for model construction on data and ANN (artificial neural network) retrieval for BP correction of radiation measurements with rough errors available,a BP model is presented.Evidence suggests that the developed model works well and is superior to a convenient multivariate linear regression model,indicating its wide applications. 相似文献
64.
The garnet-muscovite geothermometer was refined through empirical calibration by using natural rocks metamorphosed under the physical conditions of 238—1306 MPa and 490—700℃. Input temperatures and pressures were determined through simultaneously applying the garnet-biotite geothermometer and the garnet-biotite-plagioclase-quartz barometer, assuming that all FeO in muscovite and garnet be ferrous. Garnet was treated as the asymmetric quaternary solid solution, and muscovite as the symmetric binary solid solution. Input muscovite compositions include Fe atoms between 0.03—0.19 and Mg atoms between 0.04—0.16 on the basis of 11 oxygen atoms, and input garnet compositions include spessartine fractions between 0.01—0.289, grossular fractions between 0.028—0.273, and the Fe/Mg ratio between 3.387-18.986. The resulting garnet-muscovite geothermometer reproduces temperatures within (50℃ compared with the garnet-biotite thermometer. Total random error of ±37℃ of the new thermometer may stem from the pressure uncertainty of ±200 MPa, and uncertainties of ±5% of Fe and Mg components in muscovite, and ±5% of Fe, Mg, Mn and Ca components in garnet, altogether. When there exist 10%, 20%, 30%, 40% and 50% Fe3+ in muscovite, respectively, the computed garnet-muscovite temperatures will be 1—6℃, 2—12℃, 3—16℃, 5—24℃ and 7—29℃, respectively, lower than those obtained when assuming that all FeO be ferrous. The new garnet-muscovite geothermometer can efficiently reflect temperature change of typical prograde sequences and contact aureole rocks, and may be applied to low- to high-grade and low- to high-pressure metamorphic rocks. 相似文献
65.
Data and model uncertainty estimation for linear inversion 总被引:1,自引:0,他引:1
Kasper van Wijk John A. Scales William Navidi Luis Tenorio 《Geophysical Journal International》2002,149(3):625-632
66.
67.
GPS在地面沉降监测中的应用探讨 总被引:5,自引:0,他引:5
利用GPS进行地面沉降监测能够解决传统测量方法工作量大、周期长的问题。该文结合实例,论述了GPS在地面沉降监测中的应用,分析了GPS测量方法的优点和误差,提出了GPS测量地面沉降的适用条件。 相似文献
68.
69.
影像匹配技术在图像处理与计算机视觉中有着非常重要的作用。最小二乘影像匹配方法是常用的匹配方法之一。本文简单介绍了目前影像匹配的几种方法及其优缺点,探讨了数字相机的检校原理与方法。重点介绍附有约束条件的最小二乘影像匹配的原理及匹配过程,结合交通事故处理的实例,论证了该方法的可行性。与传统方法相比,在测量精度、自动化程度以及数据三维可视化等方面具有明显优势。 相似文献
70.