全文获取类型
收费全文 | 136210篇 |
免费 | 2100篇 |
国内免费 | 1098篇 |
专业分类
测绘学 | 3405篇 |
大气科学 | 9275篇 |
地球物理 | 26163篇 |
地质学 | 50066篇 |
海洋学 | 11964篇 |
天文学 | 30771篇 |
综合类 | 470篇 |
自然地理 | 7294篇 |
出版年
2022年 | 841篇 |
2021年 | 1397篇 |
2020年 | 1489篇 |
2019年 | 1675篇 |
2018年 | 4724篇 |
2017年 | 4316篇 |
2016年 | 4599篇 |
2015年 | 2154篇 |
2014年 | 3898篇 |
2013年 | 6695篇 |
2012年 | 4577篇 |
2011年 | 6563篇 |
2010年 | 5803篇 |
2009年 | 7275篇 |
2008年 | 6275篇 |
2007年 | 6644篇 |
2006年 | 5123篇 |
2005年 | 3875篇 |
2004年 | 3848篇 |
2003年 | 3719篇 |
2002年 | 3603篇 |
2001年 | 3026篇 |
2000年 | 2878篇 |
1999年 | 2338篇 |
1998年 | 2392篇 |
1997年 | 2213篇 |
1996年 | 1967篇 |
1995年 | 1914篇 |
1994年 | 1669篇 |
1993年 | 1532篇 |
1992年 | 1483篇 |
1991年 | 1484篇 |
1990年 | 1492篇 |
1989年 | 1275篇 |
1988年 | 1211篇 |
1987年 | 1387篇 |
1986年 | 1254篇 |
1985年 | 1532篇 |
1984年 | 1709篇 |
1983年 | 1589篇 |
1982年 | 1490篇 |
1981年 | 1378篇 |
1980年 | 1280篇 |
1979年 | 1240篇 |
1978年 | 1177篇 |
1977年 | 1011篇 |
1976年 | 973篇 |
1975年 | 971篇 |
1974年 | 933篇 |
1973年 | 1011篇 |
排序方式: 共有10000条查询结果,搜索用时 46 毫秒
61.
Summary Pre- to early Variscan metamorphosed volcano-sedimentary series of the western (Bergstr?sser) Odenwald have been intruded
by Variscan calc-alkaline magmatites with plate margin affinities. Within the NE-SW trending metabasic and metapelitic series,
intercalations of anomalously aluminous- and iron-rich compositions representing former bauxites are distinguishable. Geochemical
data indicate that the Al-, Fe-rich rocks are the metamorphic equivalents of a former bauxitic-ferralitic weathering profile,
now comprising spinel fels (top) with relics of pisolitic structures, corundum-chlorite fels, corundum-cordierite-plagioclase
gneiss, sillimanite-cordierite-plagioclase gneiss, cordierite-plagioclase gneiss and kinzigite (base) displaying a decrease
of weathering in the order as listed. The evolution of such terrestrial sediments is related to specific climatic, environmental,
and physico-chemical conditions similar to those of the present-day tropical to subtropical humid regions with high seasonal
rains and intensive drainage. Comparison with palaeomagnetic and palaeoclimatic data indicate that the Odenwald metabauxites
originally formed during the Lower to Mid-Devonian. Our results imply that, during this geological time span, parts of the
precursors of the Mid-German Crystalline Rise not only transversed low latitudes but also were exposed to terrestrial weathering.
Received June 10, 1999; revised version accepted October 30, 2000 相似文献
Zusammenfassung Die Geochemie der Metabauxite im Bergstr?sser Odenwald (Mitteldeutsche Kristallinschwelle) und ihre Bedeutung für das Pal?omilieu Im westlichen (Bergstr?sser) Odenwald intrudierten variszische Plattenrand-Kalkalkali-Magmatite in pr?- bis früh-variszische, ehemalige vulkano-sediment?re Serien. Innerhalb der heute NE-SW streichenden Metabasit- und Metapelitzüge treten lokal Al-Fe-reiche Einschaltungen auf, die strukturell und geochemisch als metamorphe ?quivalente eines ehemaligen bauxitisch-ferralitischen Verwitterungsprofils klassifiziert werden k?nnen. Sie umfassen Spinellfelse mit erhaltenen, ehemaligen zonierten Pisolithen, Korund-Chloritfelse, Korund-Cordierit-Plagioklasgneise, Sillimanit-Cordierit-Plagioklasgneise, Cordierit-Plagioklasgneise und Kinzigite. Bauxite k?nnen als terrestrische Bildungen nur unter speziellen klimatischen und physiko-chemischen Bedingungen entstehen. Pal?omagnetische und pal?oklimatische Daten legen die Bildung der ehemaligen Bauxite im unteren bis mittleren Devon nahe. Daraus folgt, da? w?hrend dieser geologischen Zeitspanne die Vorl?ufer der mitteldeutschen Kristallinschwelle bei der Norddrift nicht nur ?quatorn?he passierten, sondern auch partiell ungest?rte, terrestrische, tropisch-subtropische Verwitterungsprozesse abliefen.
Received June 10, 1999; revised version accepted October 30, 2000 相似文献
62.
Summary. Asymptotic ray theory (ART) fails in transition regions near critically reflected, bottom glancing or caustic-forming rays in a vertically inhomogeneous layered earth. These deficiencies are repaired here by replacing the transitional ray fields with guided modes plus truncation remainders. Exact ray-mode equivalences and their high-frequency asymptotic approximations are formulated, and their validity and efficiency are verified by numerical comparisons for SH motion in a two-layer earth model comprised of an inhomogeneous sediment above an homogeneous semi-infinite bedrock. 相似文献
63.
Similarity solutions, describing the flow of a perfect gas behind spherical shock waves, are investigated including the radiation heat flux. The shock is assumed to be propagating in a medium at rest. Shock radius varies exponentially with time and density is inversely proportional to fifth power of the shock radius immediately ahead of the shock front. 相似文献
64.
65.
66.
Homogenous isotropic cosmologies in the presence of a cosmological constant A are studied in the modified Brans-Dicke theory.
A class of exact solutions are obtained in Dicke's revised units for empty space as well as for the models filled with dust
or radiation. Behaviour of these models near the singularity are discussed. 相似文献
67.
In connection with the celebration of the centennial of the Institute of Electrical and Electronics Engineers (UEEE) in 1984, the history of electrical engineering in relation to the world's oceans is traced, with emphasis on the 20-year period from the 1960's to the present. Note is taken of the breadth of the cross-disciplinary interests involved, as exemplified by the active participation of a score of IEEE Societies and Professional Groups, how they organized to cooperate, the periodic meetings and annual conferences they sponsored, the publications they undertook, the tokens of recognition they adopted, and how they adapted to changes in emphasis to reflect shifts in the areas of technology served. Finally, an assessment is made of the future of the recently organized IEEE Oceanic Engineering Society. 相似文献
68.
Howard J. Falcon-Lang William A. DiMichele Scott Elrick & W. John Nelson 《Geology Today》2009,25(5):181-184
The development of coal forests during the Carboniferous is one of the best-known episodes in the history of life. Although often reconstructed as steamy tropical rainforests, these ancient ecosystems were a far cry from anything we might encounter in the Amazon today. Bizarre giant club-mosses, horsetails and tree ferns were the dominant plants, not flowering trees as in modern rainforests. At their height, coal forests stretched all the way from Kansas to Kazakhstan, spanning the entire breadth of tropical Pangaea. Most of what we know of their biodiversity and ecology has been quite literally mined out of the ground through two centuries of hard labour. Without coal mining, our knowledge would be greatly impoverished. Over the past few years, we've been exploring underground coal mines in the United States, where entire forested landscapes have been preserved intact over huge areas. Never before have geologists had the opportunity to walk out through mile upon mile of fossilized forest. In this feature article, we describe some of our recent explorations and attempt to shed new light on these old fossils. 相似文献
69.
Maarten A. Prins Hongbo Zheng Kay Beets Simon Troelstra Patrick Bacon Ilse Kamerling Wouter Wester Martin Konert Xiangtong Huang Wang Ke Jef Vandenberghe 《第四纪科学杂志》2009,24(1):75-84
The Mangshan Plateau is located on the south bank of the Huang He (Yellow River) just west of the city of Zhengzhou, well outside the Loess Plateau in central China. Mixing models of the grain‐size data indicate that the loess deposits are mixtures of three loess components. Comparison of the mixing model with existing models established for a series of loess–palaeosol sequences from the Loess Plateau indicates that the Mangshan loess has been supplied from a proximal dust source, the Huang He floodplain, during major dust outbreaks. The high accumulation rates, the composition of the loess components, and especially the high proportions of a sandy loess component support this. Owing to the exceptionally high accumulation rates, the Mangshan grain size, magnetic susceptibility and carbonate records provide a high‐resolution archive of environmental and climate change. Copyright © 2008 John Wiley & Sons, Ltd. 相似文献
70.
The aim of this paper is to investigate the thermal stability of a fluid layer with permeable boundaries and a variable gravitational field. It is observed that the principle of exchange of stabilities is valid when the layer is heated form below and the complex growth rate of an arbitrary oscillatory mode exists outside of a circle whose radius depends upon the permeability parameter, Prandtl number and wavelength of the mode. In the case of a layer heated from below, gravity increasing upward has a destabilizing effect whereas the permeability parameter has a stabilizing effect. 相似文献