全文获取类型
收费全文 | 66188篇 |
免费 | 1125篇 |
国内免费 | 493篇 |
专业分类
测绘学 | 1635篇 |
大气科学 | 5277篇 |
地球物理 | 13729篇 |
地质学 | 21412篇 |
海洋学 | 5718篇 |
天文学 | 15216篇 |
综合类 | 133篇 |
自然地理 | 4686篇 |
出版年
2020年 | 474篇 |
2019年 | 495篇 |
2018年 | 934篇 |
2017年 | 916篇 |
2016年 | 1363篇 |
2015年 | 1013篇 |
2014年 | 1414篇 |
2013年 | 3236篇 |
2012年 | 1491篇 |
2011年 | 2273篇 |
2010年 | 1939篇 |
2009年 | 2917篇 |
2008年 | 2661篇 |
2007年 | 2392篇 |
2006年 | 2457篇 |
2005年 | 2132篇 |
2004年 | 2238篇 |
2003年 | 2059篇 |
2002年 | 1964篇 |
2001年 | 1774篇 |
2000年 | 1746篇 |
1999年 | 1504篇 |
1998年 | 1490篇 |
1997年 | 1481篇 |
1996年 | 1273篇 |
1995年 | 1208篇 |
1994年 | 1090篇 |
1993年 | 994篇 |
1992年 | 943篇 |
1991年 | 801篇 |
1990年 | 1008篇 |
1989年 | 848篇 |
1988年 | 752篇 |
1987年 | 926篇 |
1986年 | 816篇 |
1985年 | 1019篇 |
1984年 | 1181篇 |
1983年 | 1123篇 |
1982年 | 1016篇 |
1981年 | 976篇 |
1980年 | 833篇 |
1979年 | 815篇 |
1978年 | 867篇 |
1977年 | 787篇 |
1976年 | 749篇 |
1975年 | 695篇 |
1974年 | 703篇 |
1973年 | 708篇 |
1972年 | 440篇 |
1971年 | 385篇 |
排序方式: 共有10000条查询结果,搜索用时 0 毫秒
861.
The Håkon Mosby Mud Volcano (HMMV) is a seafloor mud volcano, having a 1-km-diameter circular shape and a relief of 8–10?m. HMMV is located within a slide scar on the Bjørnøya glacial submarine fan on the SW Barents Sea slope, and is underlain by a >6-km-thick Cenozoic sequence. Multichannel seismic data reveal a 1- to 2-km-wide disturbed zone, which extends to a depth of >3?km below the HMMV. We relate the zone to the presence of free gas. The seismic data are compatible with an intrasedimentary sourced mud volcano related to the glacial sedimentation history and mass movements. 相似文献
862.
Monthly Variations of Water Masses in the Yellow and East China Seas, November 6, 1998 总被引:4,自引:0,他引:4
The monthly water mass variations in the Yellow Sea and the East China Sea are investigated using over 40 years of historical
temperature and salinity observations via a cluster analysis that incorporates geographical distance and depth separation
in addition to the temperature and salinity. Results delineate monthly variations in the major water masses and provide some
insight into formation mechanisms and intermixing. The major water masses include the Kuroshio-East China Sea water (KE),
the Yellow Sea surface water (YSS) and bottom cold water (YSB), mixed water (MW), and coastal water (CW). The distribution
of the KE water mass reveals the intrusion pattern into the area west of Cheju. A separate mixed water type appears between
the KE water mass and the Yellow Sea water masses during winter. The formation mechanism of the YSB appears to be the surface
cooling and active mixing in winter. In the East China Sea, during summer, surface water is differentiated from the subsurface
water while there is no differentiation during winter. In the Yellow Sea, a three layer system exists in the summer and fall
(May–November) while a two layer system exists during the rest of the year. A fresh water mass generated by Yangtze River
discharge (YD) is present over the northern East China Sea and the southern Yellow Sea during summer.
This revised version was published online in August 2006 with corrections to the Cover Date. 相似文献
863.
Scanning and transmission electron microscopic analyses of shale samples from offshore Louisiana, USA, Gulf of Mexico, reveal
the relationship between mineralogical and microfabric changes during burial diagenesis. The local geopressured zone begins
at 2200-m depth. Above that depth the shales are smectite-rich, generally lack particle orientation, and contain appreciable
pores. Below the 2200-m depth, the shales become more illite-rich with increasing burial, more crystalline, and less porous.
Microfabric changes are mainly caused by compaction during burial diagenesis; mineralogical changes (smectite-to-illite) and
crystal growth also play an important role in fabric alteration during deep burial diagenesis.
Received: 12 May 1998 / Revision received: 14 July 1998 相似文献
864.
Cessation of the Norwegian drift net fishery: changes observed in Norwegian and Russian populations of Atlantic salmon 总被引:1,自引:2,他引:1
865.
Management of summer-spawning herring off Iceland 总被引:1,自引:0,他引:1
866.
D. J. Staples 《新西兰海洋与淡水研究杂志》2013,47(3):365-374
Growth of the red gurnard, Chelidonichthys kumu (Lesson and Garnot), from Pegasus Bay, Canterbury, was measured during 1966–67. Otoliths were used as an indicator of fish growth; mean length‐at‐age data were obtained from back‐calculated fish lengths at the time of formation of successive annual rings in the otoliths. Growth in length was found to be adequately expressed by the von Bertalanffy growth equation : lt = 52.0 [1 ‐ e‐0.406 (t‐o.291)] (where lt is the fork length in cm at age t). The length: weight relationship was: w = 78.56 × 10‐4 l 3.072 (where w is the weight in grams). From this relationship, growth in weight was described by the equation: wt = 1469 [1 ‐ e‐0.406 (t‐0.291)]3. 相似文献
867.
F. J. Taylor 《新西兰海洋与淡水研究杂志》2013,47(2):389-402
Ten samples of freshwater from Campbell Island were analysed for their main ionic constituents. All show a preponderance of sodium and chloride derived from sea water. Potassium, calcium, and magnesium gave slightly higher concentrations than would be expected if derived solely from sea water. It is con‐eluded that the excess potassium is derived from the underlying rocks and soil, and the excess calcium and magnesium from the sea by fractionation into salt particles. 相似文献
868.
Fry of grass carp, Ctenopharyngodon idella (Val.), were air‐freighted from Hong Kong to New Zealand in October 1971. The fish were at first kept in tanks with a recirculating water supply, where they soon showed symptoms of parasitic infestation and suffered heavy mortality. Attempts were made to remove parasites with chemotherapeutic treatment. Tripartiella sp., Dactylogyrus ctenopharyngodonis, and Gyrodactylus clenopharyngodontis were eliminated by prolonged bathing of the infected fish with quinine. Chemical treatment failed to eliminate Ichthyophthirius mullifiliis from the body surface and the gills, but the rate of spontaneous recovery of the fish from this disease was accelerated by keeping them in clean, running water. Experiments to remove the cestode Bothriocephalus gowkongensis from the intestine of the fish with tetravalent tin compounds and to control the intermediate host (Cyclops) in the water resulted in the eradiction of the cestode. When parasitic infestations had been brought under control the fish were transferred to outdoor ponds, where they began to feed on aquatic and terrestrial vegetation and rapidly increased in size. 相似文献
869.
870.
Angela J. Ramsay 《新西兰海洋与淡水研究杂志》2013,47(1):77-90
The viable heterotrophic bacteria of Lake Grasmere in inland Canterbury (43° 05 S, 171° 45 E) were studied. Numbers of bacteria in water above a spring were positively correlated with rainfall in the 7 days before sampling, but bacteria in open water and from over the macrophyte Elodea canadensis were not. There was some increase in the bacterial population in the water over E. canadensis in the autumn to winter months. Numbers of bacteria in the open water ranged from 55 to 1020 cells per millilitre, and were outnumbered by algae by a factor of between 4 and 34. The bacterial population tended to increase after blooms of zooplankton, but there was little or no response to changes in phytoplankton populations. Benthic bacteria rarely increased in numbers after the deposition of organic matter. 相似文献