全文获取类型
收费全文 | 1162篇 |
免费 | 46篇 |
国内免费 | 19篇 |
专业分类
测绘学 | 20篇 |
大气科学 | 102篇 |
地球物理 | 293篇 |
地质学 | 383篇 |
海洋学 | 126篇 |
天文学 | 183篇 |
综合类 | 7篇 |
自然地理 | 113篇 |
出版年
2021年 | 14篇 |
2020年 | 13篇 |
2019年 | 21篇 |
2018年 | 28篇 |
2017年 | 20篇 |
2016年 | 29篇 |
2015年 | 26篇 |
2014年 | 38篇 |
2013年 | 59篇 |
2012年 | 42篇 |
2011年 | 38篇 |
2010年 | 40篇 |
2009年 | 56篇 |
2008年 | 51篇 |
2007年 | 39篇 |
2006年 | 43篇 |
2005年 | 36篇 |
2004年 | 24篇 |
2003年 | 41篇 |
2002年 | 24篇 |
2001年 | 32篇 |
2000年 | 28篇 |
1999年 | 19篇 |
1998年 | 20篇 |
1997年 | 17篇 |
1996年 | 9篇 |
1995年 | 14篇 |
1994年 | 17篇 |
1993年 | 19篇 |
1992年 | 8篇 |
1991年 | 13篇 |
1990年 | 19篇 |
1989年 | 15篇 |
1987年 | 12篇 |
1986年 | 7篇 |
1985年 | 20篇 |
1984年 | 18篇 |
1983年 | 19篇 |
1982年 | 30篇 |
1981年 | 24篇 |
1980年 | 22篇 |
1979年 | 20篇 |
1978年 | 18篇 |
1977年 | 21篇 |
1976年 | 18篇 |
1975年 | 13篇 |
1974年 | 16篇 |
1973年 | 18篇 |
1972年 | 6篇 |
1971年 | 8篇 |
排序方式: 共有1227条查询结果,搜索用时 15 毫秒
361.
A visual albedo distribution model for all hemispheres of Io's surface has been synthesized from available Earth-based and spacecraft image and photometric data. The resulting model indicates some interesting patterns and symmetries on Io's surface: The dark polar caps are shifted off Io's rotational axis and are eliptical rather than circular in shape, with extensions toward the sub-Jupiter and anti-Jupiter points on Io; equatorial bright areas are located approximately on a great circle about Io, the plane of which is tilted approximately 15° toward Io longitude 60°. These and other indicated features may be clues to understanding the endogenic and exogenic processes that have resulted in Io's present observed surface characteristics. 相似文献
362.
363.
P. G. Johnson 《Astrophysics and Space Science》1982,82(1):213-221
A new series of ultra-deep, wide-angle H filter photographs at higher angular resolution than hitherto achieved, have been obtained covering the Orion-Taurus-Eridanus region. These reveal new, both diffuse and filamentary nebulosities near the Barnard Arc Nebula, which are correlated with Hi features in the region. Mechanisms capable of producing the observed features are discussed. Both a stellar wind bubble and a fossil supernova remnant are considered possible explanations, and would represent the nearest examples of these features to the Sun. Furthermore, nebulosity in this region has been photographed for the first time at [Nii]. The possible implications of this and other observations are discussed. 相似文献
364.
LIU Xiao-bing Elizabeth J.Johnson Peter L.M.Veneman XING Baos-han 《湿地科学》2003,1(2):128-135
Wetlands, one of the most productive systems in the biosphere are a unique ecosystem. They occur in landscapes that favor the ponding or slow runoff of surface water, discharge of ground water, or both. Wetlands are not only important for maintaining plant and animal diversity, but also for balancing global carbon budget via sequestrating or releasing CO2 from/into atmosphere depending on their management. Therefore, it is imperative to understand how wetlands form and function, then we can better manage, utilize, and protect these unique ecosystems. Hydric soils, hydrophytic vegetation, and wetland hydrology are the three main parameters of wetlands. These parameters are interrelated with each other which jointly influence the development and functions of wetland ecosystems. The objective of this paper was to report the current understanding of wetlands and provide future research directions. The paper will first focus on aspects of hydrology research in wetlands, and then shift to soil hydrosequence a 相似文献
365.
K. Johnson C. Barnes J. Browning H. Karlsson 《Contributions to Mineralogy and Petrology》2002,142(5):564-581
The Middle Cretaceous Cornucopia stock in the Blue Mountains of northeastern Oregon is a small composite intrusion consisting of hornblende biotite tonalite, biotite trondhjemite, and three cordierite two mica trondhjemite units. Unusual magnetite + biotite-rich tonalitic rocks are associated with the Crater Lake cordierite trondhjemite, the youngest of the intrusions. Oxide-rich tonalites are characterized by high Fe (~47-68 wt% total Fe as FeO), low SiO2 (<36 wt%), and enrichments in HFSE and REE (La(N)=361-903). Oxide-rich tonalites appear in a variety of forms, including composite dikes and sheets, in which they are associated with leucocratic tonalite. Leucotonalite is lower in SiO2 (60-72 wt%) than Crater Lake trondhjemite, and generally has DREE contents and Eu anomalies intermediate between the oxide-rich tonalite and Crater Lake compositions. Oxide-rich tonalites crosscut, and are crosscut by, shear zones in the host trondhjemite, indicating their emplacement late in the pluton's crystallization history. Granitic dikes crosscut the composite dikes in all localities. Geochemical considerations and sedimentary-like structures, such as load casts and bedding of magnetite-rich assemblages in the composite dikes and sheets, are suggestive of crystal settling from an Fe-rich parental magma. The Fe-rich liquid parental to the oxide-rich tonalite-leucotonalite pairs formed by extensive, in-situ, plagioclase + quartz-dominated crystallization of strongly peraluminous trondhjemite. Early magnetite saturation in the trondhjemite was suppressed, either because the parental trondhjemitic magma had a lower initial total Fe content or because it had a lower ferric-ferrous ratio, possibly reflecting a lower oxygen fugacity. Accumulation of magnetite from Fe-rich residual magma is a viable mechanism for the concentration of iron, and the subsequent formation of Fe-rich rocks, in calcic siliceous intrusions. Apparently, Fe-enrichment can occur locally in calcic magmas, and is not restricted to rocks of mafic tholeiitic or anorthositic affinity. 相似文献
366.
Annual sediment budget of a UK mountain torrent 总被引:2,自引:0,他引:2
Richard M. Johnson & Jeff Warburton 《Geografiska Annaler: Series A, Physical Geography》2002,84(2):73-88
Research into torrent erosion focuses heavily on bedload transport dynamics and debris flow propagation during specific events. As a result, there is limited understanding of the sediment budgets operating in torrent systems over longer timescales. The aim of this study is to construct a sediment budget of the main geomorphological processes operating in a mountain torrent sediment system over a full year.
The study site is Iron Crag which is a small torrent system (catchment area 2.4 ha) situated in the northern Lake District, UK. The site has the characteristic morphology of a torrent: multiple hillslope sediment sources, steep channel, gorges, and a basal alluvial fan. A measurement scheme was designed to monitor process activity, linking the sediment sources and sinks, from December 1998 to December 1999. Over this time period the sediment budget demonstrates that 184 tonnes of sediment was supplied to the alluvial fan (which acted primarily as a sediment sink). Channel (70%) and bank (25%) sources dominated the sediment supply, and surface processes and rockfall on the hillslopes (5%) made only a minor contribution.
Temporal variations in process activity are significant. Surface processes and rockfall display seasonal variations in yield, whilst channel and bank yields are influenced by individual storm events. Site–specific meteorological data are used to explain these observations and freeze–thaw activity and rainfall characteristics are shown to be important controlling factors. 相似文献
The study site is Iron Crag which is a small torrent system (catchment area 2.4 ha) situated in the northern Lake District, UK. The site has the characteristic morphology of a torrent: multiple hillslope sediment sources, steep channel, gorges, and a basal alluvial fan. A measurement scheme was designed to monitor process activity, linking the sediment sources and sinks, from December 1998 to December 1999. Over this time period the sediment budget demonstrates that 184 tonnes of sediment was supplied to the alluvial fan (which acted primarily as a sediment sink). Channel (70%) and bank (25%) sources dominated the sediment supply, and surface processes and rockfall on the hillslopes (5%) made only a minor contribution.
Temporal variations in process activity are significant. Surface processes and rockfall display seasonal variations in yield, whilst channel and bank yields are influenced by individual storm events. Site–specific meteorological data are used to explain these observations and freeze–thaw activity and rainfall characteristics are shown to be important controlling factors. 相似文献
367.
The High Plains are a vast, low relief landscape that contains thousands of upland-embedded depressional playa wetlands. Lunettes are isolated dunes that form from prolonged periods of aeolian deposition along the downwind margin of some larger playas. Playa-lunette systems are important landscape elements that have the potential to preserve high-resolution records of past environments, and several archeological sites have been associated with playa-lunette systems throughout the High Plains. While a comprehensive playa wetland geospatial database has been developed for the High Plains, lunettes have only been mapped for the Southern High Plains of Texas and New Mexico. The purpose of this research was to map and characterize the geomorphology of all lunettes associated with playas in the High Plains and bordering regions of western Kansas. Results indicate 129 lunettes are associated with 104 playas in Kansas. All lunettes are associated with playas larger than 5 ha, and about 10% of these larger playas have a lunette. Lunette height ranges from approximately 1.5–12 m, with a median height of 3 m. Most lunettes (60%) are in Finney, Gray, Lane, and Scott counties, which have broad, flat uplands with few major drainages upwind of playas and lunettes. 相似文献
368.
Briana E. Johnson Paula J. Noble Alan C. Heyvaert Sudeep Chandra Robert Karlin 《Journal of Paleolimnology》2018,59(2):159-173
This study addresses the effects of climate, land-use, and atmospheric nitrogen (N) deposition on the Fallen Leaf Lake watershed, Lake Tahoe Basin, through diatom and geochemical analyses of sediment cores. Four diatom zones are recognized from a core taken at Fallen Leaf Lake (FLL), a site moderately impacted by human activities: (1) Pre-Little Ice Age Zone (840–1385), (2) Little Ice Age Zone (1385–1810) characterized by Stephanodiscus alpinus and Aulacoseira subarctica, (3) Transitional Zone (1810–1950) of warming and anthropogenic influence with increased Lindavia rossii-ocellata group and Discostella stelligera and decreased Pseudostaurosira brevistriata, and (4) Anthropogenic Zone (1950–2010) characterized by a rapid increase of mesotrophic diatoms of the Fragilaria tenera-nanana group, Tabellaria flocculosa strain IIIP, and Nitzschia gracilis. The Transitional Zone increases in elemental Co, Zn, and Sn that may be attributed to an increase in coal burning and smelting activities in California and Nevada. Beginning around 1910 and accelerating in the 1940s, increased building, land-use, and recreation around FLL caused an increase in terrestrial sedimentary input. Down core proxies for atmospheric N deposition in the FLL watershed are, at best, weakly expressed and appear to be overshadowed by stronger signals. Lack of support for N deposition includes the asynchrony in the appearance of the N-sensitive diatom Asterionella formosa in FLL and a lower impact site at Gilmore Lake, and an uninformative δ15N record. Asterionella formosa is a dominant component in the FLL water column today, but has been present in similar abundances for at least the last 1200 years. Asterionella formosa is present in the water column at Gilmore Lake and absent from the sediment, indicating a very recent appearance. The data collected show that the FLL record is sensitive to climatic cooling during the Little Ice Age and to anthropogenic activities commencing in the 1800s that increased throughout the latter half of the twentieth century; however the effects of anthropogenic N deposition in these lakes could not be substantiated. 相似文献
369.
The cartogram, or value-by-area map, is a popular technique for cartographically representing social data. Such maps visually equalize a basemap prior to mapping a social variable by adjusting the size of each enumeration unit by a second, related variable. However, to scale the basemap units according to an equalizing variable, cartograms must distort the shape and/or topology of the original geography. Such compromises reduce the effectiveness of the visualization for elemental and general map-reading tasks. Here we describe a new kind of representation, termed a value-by-alpha map, which visually equalizes the basemap by adjusting the alpha channel, rather than the size, of each enumeration unit. Although not without its own limitations, the value-by-alpha map is able to circumvent the compromise inherent to the cartogram form, perfectly equalizing the basemap while preserving both shape and topology. 相似文献
370.