全文获取类型
收费全文 | 40768篇 |
免费 | 2135篇 |
国内免费 | 3913篇 |
专业分类
测绘学 | 2317篇 |
大气科学 | 4415篇 |
地球物理 | 7733篇 |
地质学 | 19835篇 |
海洋学 | 3317篇 |
天文学 | 3471篇 |
综合类 | 3011篇 |
自然地理 | 2717篇 |
出版年
2024年 | 115篇 |
2023年 | 322篇 |
2022年 | 739篇 |
2021年 | 966篇 |
2020年 | 857篇 |
2019年 | 890篇 |
2018年 | 5734篇 |
2017年 | 4936篇 |
2016年 | 3496篇 |
2015年 | 990篇 |
2014年 | 1065篇 |
2013年 | 1060篇 |
2012年 | 1981篇 |
2011年 | 3768篇 |
2010年 | 2959篇 |
2009年 | 3215篇 |
2008年 | 2732篇 |
2007年 | 3230篇 |
2006年 | 859篇 |
2005年 | 623篇 |
2004年 | 760篇 |
2003年 | 824篇 |
2002年 | 742篇 |
2001年 | 498篇 |
2000年 | 391篇 |
1999年 | 377篇 |
1998年 | 306篇 |
1997年 | 308篇 |
1996年 | 258篇 |
1995年 | 256篇 |
1994年 | 232篇 |
1993年 | 182篇 |
1992年 | 164篇 |
1991年 | 110篇 |
1990年 | 95篇 |
1989年 | 111篇 |
1988年 | 79篇 |
1987年 | 63篇 |
1986年 | 57篇 |
1985年 | 46篇 |
1984年 | 42篇 |
1983年 | 41篇 |
1982年 | 41篇 |
1981年 | 47篇 |
1980年 | 43篇 |
1979年 | 29篇 |
1977年 | 17篇 |
1976年 | 22篇 |
1975年 | 22篇 |
1973年 | 17篇 |
排序方式: 共有10000条查询结果,搜索用时 0 毫秒
141.
On the basis of the observation data of Kuroshio since 1984 and relative historical data in the East China Sea, spatial and temporal variation of water mass mixing characteristic in the observation area is analysed. The main results are as follows. 相似文献
142.
INTRODUCTIONTheDenglouCape ,inthesouthwestoftheLeizhouPeninsula ,isatthenorthmarginoftropicalzone .SeveralresearchesandcartographiesoftheregionalgeomorphologyandQuater narygeology ,whichwerecarriedoutinthepast,allincludethisarea (MGL ,SCSIO ,CAS ,1 978;GPCSGRCZT… 相似文献
143.
中国沿岸现代海平面变化及未来趋势分析 总被引:2,自引:0,他引:2
本文用线性回归分析方法,分1985年以前和1992年以前两个时段,对我国沿岸25个验潮站近百年来的海平面资料进行了系统分析,计算了两个时段相对海平面变化的年速率和平均海面高度,论述了海平面变化的主要控制因素,并对未来海平面变化趋势进行了预测。计算结果表明,近百年来我国沿岸相对海平面在总体上不但持续上升,而且近年来上升速率普遍加快;根据海平面变化的主要控制因素变化趋向,预计到下世纪中叶前后,全球性海平面大幅度上升的可能性不大,我国沿岸区域性海乎面平均上升幅度不超过15cm,不同岸段因地壳升降差异性大而有较大差别。 相似文献
144.
145.
146.
Two genetically different types of authigenic carbonate mounds are studied: those within an active hydrothermal field related to serpentinite protrusions in the zone of intersection of a transform fracture zone and the Mid-Atlantic Ridge, and those in an active field of methane seepings in the Dnieper canyon of the Black sea. The general geochemical conditions under which authigenic carbonate formation occurs in the two fields considered were found. They include the presence of reduced H2S, H2, and CH4 gases at the absence of free oxygen; the high alkalinity of the waters participating in the carbonate formation; the similarity of the textural and structural features of authigenic aragonite, which represents the initial mineral of the carbonate matter of the mounds; the paragenesis of aragonite with sulfide minerals; and the close relation of carbonate mounds with communities of sulfate-reducing and methane-oxidizing microorganisms. A new mechanism of formation of hydrothermal authigenic carbonates is suggested; it implies their microbial sulfate reduction over the hydrogen of the fluid in the subsurface zone (biosphere) of mixing between the hydrothermal solution and the adjacent seawater. 相似文献
147.
INTRODUCTION Sea urchin is a marine animal of economic value. The gonad of Hemicentrotus pulcherrimus A. Agassiz and Anthocidaris crassispina A. Agassiz may be offered as food and medicine, the sea urchin shell may be used as fertilizer and artware and moreover, the sea urchin eggs are important materials for the studies in embryology and molecular biology. With the increasing exportation of sea urchins in China, the natural resources are gradually decreasing. In order to satisfy people's growing needs of sea 相似文献
148.
149.
The Magellan seamounts began forming as large submarine shield volcanoes south of the equator during the Cretaceous. These
volcanoes formed as a cluster on the small Pacific plate in a period when tectonic stress was absent. Thermal subsidence of
the seafloor led to sinking of these volcanoes and the formation of guyots as the seamounts crossed the equatorial South Pacific
(10–0°S) sequentially and ocean surface temperatures became too high for calcareous organisms to survive. Guyot formation
was completed between about 59 and 45 Ma and the guyots became phosphatized at about 39–34 and 27–21 Ma. Ferromanganese crusts
began formation as proto-crusts on the seamounts and guyots of the Magellan Seamount cluster towards the end of the Cretaceous
up to 55 Ma after the formation of the seamounts themselves. The chemical composition of these crusts evolved over time in
a series of steps in response to changes in global climate and ocean circulation. The great thickness of these crusts (up
to 15–20 cm) reflects their very long period of growth. The high Co contents of the outer parts of the crusts are a consequence
of the increasing deep circulation of the ocean and the resulting deepening of the oxygen minimum zone with time. Growth of
the Co-rich Mn crusts in the Magellan Seamount cluster can be considered to be the culmination of a long journey through time. 相似文献
150.
Ryoko Tokeshi Kaoru Ichikawa Satoshi Fujii Kenji Sato Shoichiro Kojima 《Journal of Oceanography》2007,63(4):711-720
A method to extract geostrophic current in the daily mean HF radar data in the Kuroshio upstream region is established by
comparison with geostrophic velocity determined from the along-track altimetry data. The estimated Ekman current in the HF
velocity is 1.2% (1.5%) and 48° (38°)-clockwise rotated with respect to the daily mean wind in (outside) the Kuroshio. Furthermore,
additional temporal smoothing is found necessary to remove residual ageostrophic currents such as the inertial oscillation.
After removal of the ageostrophic components, the HF geostrophic velocity agrees well with that from the altimetry data with
rms difference 0.14 (0.12) m/s in (outside) the Kuroshio. 相似文献