全文获取类型
收费全文 | 1808篇 |
免费 | 81篇 |
国内免费 | 6篇 |
专业分类
测绘学 | 76篇 |
大气科学 | 136篇 |
地球物理 | 388篇 |
地质学 | 715篇 |
海洋学 | 134篇 |
天文学 | 288篇 |
综合类 | 8篇 |
自然地理 | 150篇 |
出版年
2024年 | 5篇 |
2023年 | 12篇 |
2022年 | 10篇 |
2021年 | 30篇 |
2020年 | 46篇 |
2019年 | 44篇 |
2018年 | 55篇 |
2017年 | 77篇 |
2016年 | 90篇 |
2015年 | 60篇 |
2014年 | 58篇 |
2013年 | 119篇 |
2012年 | 79篇 |
2011年 | 96篇 |
2010年 | 108篇 |
2009年 | 99篇 |
2008年 | 102篇 |
2007年 | 90篇 |
2006年 | 92篇 |
2005年 | 84篇 |
2004年 | 87篇 |
2003年 | 58篇 |
2002年 | 61篇 |
2001年 | 35篇 |
2000年 | 23篇 |
1999年 | 38篇 |
1998年 | 20篇 |
1997年 | 15篇 |
1996年 | 17篇 |
1995年 | 6篇 |
1994年 | 21篇 |
1993年 | 14篇 |
1992年 | 7篇 |
1991年 | 7篇 |
1990年 | 8篇 |
1989年 | 7篇 |
1988年 | 5篇 |
1987年 | 8篇 |
1986年 | 5篇 |
1985年 | 8篇 |
1984年 | 6篇 |
1983年 | 10篇 |
1982年 | 7篇 |
1981年 | 8篇 |
1980年 | 15篇 |
1979年 | 7篇 |
1978年 | 5篇 |
1977年 | 6篇 |
1976年 | 6篇 |
1974年 | 4篇 |
排序方式: 共有1895条查询结果,搜索用时 15 毫秒
111.
Do diatoms in the Swiss Alps reflect the length of ice-cover? 总被引:11,自引:0,他引:11
112.
R. A. Leske C. M. S. Cohen R. A. Mewaldt E. R. Christian A. C. Cummings A. W. Labrador E. C. Stone M. E. Wiedenbeck T. T. von Rosenvinge 《Solar physics》2012,281(1):301-318
The solar particle event observed at STEREO Ahead on 18?August 2010 displayed a rich variety of behavior in the particle anisotropies. Sectored rates measured by the Low Energy Telescope (LET) on STEREO showed very large bidirectional anisotropies in 4??C?6?MeV protons for the first ???17?hours of the event while inside a magnetic cloud, with intensities along the field direction several hundred to nearly 1000 times greater than those perpendicular to the field. At the trailing end of the cloud, the protons became isotropic and their spectrum hardened slightly, while the He/H abundance ratio plunged by a factor of approximately four for about four hours. Associated with the arrival of a shock on 20?August was a series of brief (<?10?minute duration) intensity increases (commonly called ??shock spikes??) with relatively narrow angular distributions (???45° FWHM), followed by an abrupt decrease in particle intensities at the shock itself and a reversal of the proton flow to a direction toward the Sun and away from the receding shock. We discuss the STEREO/LET observations of this interesting event in the context of other observations reported in the literature. 相似文献
113.
WASP-1b and WASP-2b: two new transiting exoplanets detected with SuperWASP and SOPHIE 总被引:1,自引:0,他引:1
A. Collier Cameron F. Bouchy G. Hébrard P. Maxted D. Pollacco F. Pont I. Skillen B. Smalley R. A. Street R. G. West D. M. Wilson S. Aigrain D. J. Christian W. I. Clarkson B. Enoch A. Evans A. Fitzsimmons M. Fleenor M. Gillon C. A. Haswell L. Hebb C. Hellier S. T. Hodgkin K. Horne J. Irwin S. R. Kane F. P. Keenan B. Loeillet T. A. Lister M. Mayor C. Moutou A. J. Norton J. Osborne N. Parley D. Queloz R. Ryans A. H. M. J. Triaud S. Udry P. J. Wheatley 《Monthly notices of the Royal Astronomical Society》2007,375(3):951-957
We have detected low-amplitude radial-velocity variations in two stars, USNO-B1.0 1219–0005465 (GSC 02265–00107 = WASP–1 ) and USNO-B1.0 0964–0543604 (GSC 00522–01199 = WASP–2 ). Both stars were identified as being likely host stars of transiting exoplanets in the 2004 SuperWASP wide-field transit survey. Using the newly commissioned radial-velocity spectrograph SOPHIE at the Observatoire de Haute-Provence, we found that both objects exhibit reflex orbital radial-velocity variations with amplitudes characteristic of planetary-mass companions and in-phase with the photometric orbits. Line-bisector studies rule out faint blended binaries as the cause of either the radial-velocity variations or the transits. We perform preliminary spectral analyses of the host stars, which together with their radial-velocity variations and fits to the transit light curves yield estimates of the planetary masses and radii. WASP-1b and WASP-2b have orbital periods of 2.52 and 2.15 d, respectively. Given mass estimates for their F7V and K1V primaries, we derive planet masses 0.80–0.98 and 0.81–0.95 times that of Jupiter, respectively. WASP-1b appears to have an inflated radius of at least 1.33 R Jup , whereas WASP-2b has a radius in the range 0.65–1.26 R Jup . 相似文献
114.
Meteorite impact‐generated accretionary lapilli are not well studied. The recently discovered distal ejecta from the 1850 Ma Sudbury impact event contain abundant accretionary lapilli generated during the impact and deposited at great distances from the crater. We petrographically and geochemically examined lapilli from five sites (McClure, Connors Creek, Hwy 588, Pine River, and Grand Trunk Pacific, approximately 480–750 km from the center of the Sudbury structure). The compositions of quartz, K‐feldspar, calcite, biotite, and chlorite minerals are similar to each other in all of the samples, although the relative proportions of the minerals vary from site to site. The lapilli occur in a matrix of coarse‐grained quartz, carbonate, and feldspar grains. Zonation within lapilli appears to be due to grain size distribution rather than compositional variation. The inner zones are coarser grained than outer zones. The relative abundances of calcite, phyllosilicates, and feldspars are similar in each zone within individual lapilli. A meteoritic component is indicated by up to 1.8 ppb Ir in one lapillus from the Pine River site, and Ni and Cr ratios are on a chondritic trend line for many of the lapilli. Mechanisms previously proposed for accretionary lapilli formation seem inadequate to explain deposition of distal accretionary lapilli resulting from impact events. A new mechanism for upper atmospheric accretion is proposed, whereby ash ejected from impact events concentrates at altitudes of neutral buoyancy, where it then accretes and is deposited later than ballistically emplaced particles. Likely, multiple processes are taking place in the chaotic postimpact environment. 相似文献
115.
116.
117.
Christian J. Noll Timothy M. Dellapenna Andrea Gilkinson Randall W. Davis 《Geo-Marine Letters》2009,29(1):1-16
Surficial sediment distribution within Simpson Bay is a function of antecedent bedrock and recently deposited glacial geology,
as well as active physical processes both within Simpson Bay and Prince William Sound (PWS). Simpson Bay is a turbid, outwash
fjord located in northeastern PWS, Alaska. Freshwater from heavy precipitation, and the melting of high alpine glaciers enter
the bay through bay head rivers and small shoreline creeks. The catchment has a high watershed/basin surface area ratio (∼8:1),
and easily erodible bedrock that contribute to high sediment loads. The system can be divided into three discrete basins,
each with specific morphologic and circulatory characters. Side scan sonar, swath bathymetry, and seismic profiles reveal
that bathymetric highs are areas of outcropping glacial surfaces. High backscatter coupled with surface grab samples reveal
these surfaces to be composed of coarse sediment and bedrock outcrops. Bathymetric lows are areas of low backscatter, and
grab samples reveal these areas to be ponded deposits of organic-rich estuarine muds. The data provide evidence of terminal
morainal bank systems, and glacial grounding line deposits at the mouth of the bay and rocky outcrops were identified as subsurface
extensions of aerial rocky promontories. Radioisotope analyses of short cores reveal that the bay has an average accumulation
rate of approx. 0.5 cm year−1, but that this varies in function of the watershed/basin surface area ratios of the different basins. The interaction of
tidal currents and sediment source drives sediment distribution in Simpson Bay. Hydrographic data reveal high spatial variability
in surface and bottom currents throughout the bay. Subsurface currents are tide dominated, but generally weak (5–20 cm s−1), while faster currents are found along shorelines, outcrops, and bathymetric highs. Bathymetric data reveal steep slopes
with little to no modern sediment throughout the bay, suggesting lack of deposition due to tidal currents. 相似文献
118.
Christian Christiansen Dan Bowman 《Geografisk tidskrift / udgivet af Bestyrelsen for Det Kongelige danske geografiske selskab》2013,113(1):28-31
Christiansen, C. & Bowman, D.: Sea-level changes, coastal dune building and sand drift, North-Western Jutland, Denmark. Geografisk Tidsskrift 86: 28–31. Copenhagen, June 1986. Two main models linking dune building and sea level changes have so far been proposed. Application of the low sea level model suggests that the major Danish dune building period from 1550 to 1750 need not necessarily be the result of human activity. The dune building period is probably related to a low sea level and the reworking of exposed shallow marine sand. 相似文献
119.
Seismic anisotropy beneath Dronning Maud Land, Antarctica, revealed by shear wave splitting 总被引:1,自引:0,他引:1
Bettina Bayer Christian Müller David W. Eaton Wilfried Jokat 《Geophysical Journal International》2007,171(1):339-351
Shear wave splitting analyses have been carried out using teleseismic data from broad-band seismograph stations deployed at temporary and permanent locations in Dronning Maud Land (DML), Antarctica. In most cases, the observed anisotropy can be related to major tectonic events that formed the present-day Antarctic continent. We rule out an anisotropic contribution from recent asthenospheric flow. At the Russian base Novolazarevskaya near the coast in central DML, waveform inversion suggests a two-layer model where the fast direction of the upper layer is oriented parallel to Archean fabrics in the lithosphere, whereas the anisotropy of the lower layer is interpreted to have been created during the Jurassic Gondwana break-up. Recordings at the South African base Sanae IV, however, show enigmatic results. For narrow backazimuthal segments, splitting parameters show strong variations together with a multitude of isotropic measurements, indicative of complex scattering that cannot be explained by simple one- or two-layer anisotropic models. In the interior of the continent, the data are consistent with single-layer anisotropy, but show significant spatial variations in splitting parameters. A set of temporary stations across the Heimefront shear zone in western DML yield splitting directions that we interpret as frozen anisotropy from Proterozoic assembly of the craton. An abrupt change in fast axis direction appears to mark a suture between the Grunehogna craton, a fragment of the Kalahari–Kaapvaal craton in southern Africa and the Mesoproterozoic Maudheim Province. 相似文献
120.
Aurélien van Welden Christian Beck Jean-Louis Reyss Salvatore Bushati Rexhep Koci François Jouanne Jean-Louis Mugnier 《Journal of Paleolimnology》2008,40(2):619-633
Lake Shkodra (northern Albania, southern Montenegro) is a large (45 km length, 15 km width) and shallow (5 m mean depth) lake,
developed on a mainly karstic carbonate substratum. Its recent sedimentary fill (mixed calcareous/siliciclastic clayey silts)
was analysed through short gravity cores representing five centuries of environmental archive. A combination of high resolution
texture analysis (particle size), magnetic susceptibility, carbon content, and radionuclide activity profiles (210Pb, 137Cs, 241Am) permitted us to detect and date environmental changes, such as the Little Ice Age and the 1962–1963 catastrophic floods.
Anthropogenic influences on the watershed, such as damming of the Drin River in the late 1970s, also appear to be recorded.
Impacts of known strong earthquakes (1905, 1979), however, could not be clearly detected in the sediment record. The potential
of the Shkodra lacustrine archive for paleoseismic investigations on long time intervals (such as Holocene) is discussed.
This paper is a preliminary contribution to Shkodra Lake’s Holocene paleolimnology. 相似文献