全文获取类型
收费全文 | 108540篇 |
免费 | 1528篇 |
国内免费 | 660篇 |
专业分类
测绘学 | 2518篇 |
大气科学 | 7122篇 |
地球物理 | 20407篇 |
地质学 | 40914篇 |
海洋学 | 9423篇 |
天文学 | 24336篇 |
综合类 | 364篇 |
自然地理 | 5644篇 |
出版年
2022年 | 710篇 |
2021年 | 1173篇 |
2020年 | 1235篇 |
2019年 | 1396篇 |
2018年 | 4442篇 |
2017年 | 4017篇 |
2016年 | 3882篇 |
2015年 | 1591篇 |
2014年 | 2971篇 |
2013年 | 5110篇 |
2012年 | 3811篇 |
2011年 | 5658篇 |
2010年 | 5052篇 |
2009年 | 6223篇 |
2008年 | 5268篇 |
2007年 | 5756篇 |
2006年 | 4038篇 |
2005年 | 3018篇 |
2004年 | 2937篇 |
2003年 | 2836篇 |
2002年 | 2763篇 |
2001年 | 2282篇 |
2000年 | 2201篇 |
1999年 | 1735篇 |
1998年 | 1775篇 |
1997年 | 1658篇 |
1996年 | 1417篇 |
1995年 | 1399篇 |
1994年 | 1214篇 |
1993年 | 1128篇 |
1992年 | 1067篇 |
1991年 | 1080篇 |
1990年 | 1059篇 |
1989年 | 943篇 |
1988年 | 855篇 |
1987年 | 1026篇 |
1986年 | 896篇 |
1985年 | 1090篇 |
1984年 | 1212篇 |
1983年 | 1177篇 |
1982年 | 1083篇 |
1981年 | 1017篇 |
1980年 | 924篇 |
1979年 | 886篇 |
1978年 | 845篇 |
1977年 | 728篇 |
1976年 | 717篇 |
1975年 | 716篇 |
1974年 | 685篇 |
1973年 | 774篇 |
排序方式: 共有10000条查询结果,搜索用时 125 毫秒
891.
892.
I. Iovtschev 《Mineralium Deposita》1966,1(3):251-257
Résumé On peut, en résumé, caractériser ainsi les principales provinces de la Bulgarie: — les Rhodopes constituent une zone typiquement polymétallique avec une prépondérance soulignée de Pb, Zn; le F, Cr, Ni, y existent en quantité subordonnée; en traces viennent encore: le Ba, Mn, Cd, Sb, W, Mo, Bi, As, Au, Ag, V; — la Sredna Gora est caractérisée comme une zone de cuivre typique, avec la présence de Fe, Mn, et en quantitée subordonnée de Pb, Zn, Mo, Ti, V, Au. — les Balkans portent les particularités d'une zone polymétallique (Pb, Zn, Cu) avec fer. On y remarque souvent des gîtes individualisés de cuivre, polymétallique avec fer, argent, ainsi que des gîtes complexes. Le Mn, Ba, Au, Ag, Co, Mo, As, Hg, V, W viennent en quantité subordonnée; — la zone des Kraistides, analogue à la précédente, se caractérise par des gisements polymétalliques pauvres et des gîtes à or et scheelite. Les éléments principaux sont: Au, Ba et secondaires: Pb, Zn, Cu, V et en partie du Fe et Hg; — la plateforme mésique, outre le gaz, se caractérise par le manganèse de la dépression de Varna.
The metallogenic map of Bulgaria displays the following four major and distinct provinces: The Rhodopes as a typically polymetallic zone, mainly with Pb and Zn, but also with F, Cr and Ni, and minor or trace amounts of Ba, Mn, Cd, Sb, Mo, Bi, As, Au, Ag, V. The Sredna-gora is a distinct copper zone, with Fe and Mn, and minor amounts of Pb, Zn, Mo, Ti, V, Au. The Balkan is again a polymetallic zone of Pb, Zn and Cu with Fe; but Cu-Fe-Ag-deposits also occur. The other elements are present in minor quantities only. The Kraiste-Zone resembles the previous one and contains low grade polymetallic and scheelite deposits. The main elements are Au, Ba, and minor quantities of Pb, Zn, Cu, V and in part Fe and Hg. The zone of the Mésie platform contains only the manganese deposits of the Varna depression, in addition to natural gas.相似文献
893.
A series of exploratory experiments on the concentration of base metals through ion exchange reactions on clay minerals show promising results. The extraction of Pb, Zn and Cd from bentonite, illite, kaolinite and montmorillonite was successful and megascopic quantities of PbS, CdS and ZnS could be obtained at specific loci, depending essentially on the flow velocity, and the other cations present. These or similar exchange reactions are tentatively proposed as possible mechanisms of economic metal concentration during diagenesis.
Zusammenfassung Es werden experimentelle Resultate zur Anreicherung von Schwermetallen durch Tonminerale (Montmorillonite, Illite und Kaolinite) mitgeteilt. Eine erste Anreicherung kann über den Kationenaustausch bewirkt werden. In dem darauffolgenden zweiten, sehr viel wirksameren Schritt werden die Schwermetallionen aus den Tonlagern extrahiert und in deren Nähe als schwerlösliche Sulfide oder Carbonate gefällt. Die Extraktion beruht darauf, daß Tonschichten als Kationen-permeable Membranen wirken können. Sie wird von der Art der Tonminerale und der Kationen, den Lösungsgenossen, den Konzentrationsverhältnissen, dem pH-Wert, der Reaktionstemperatur, dem Porenvolumen und der Porenverteilung im Sediment beeinflußt.相似文献
894.
The long-wave outgoing radiation, effective cloudiness equal to the product of the total cloud amount by their optical density,
and the sea-surface temperature determined from the satellites are used to determine the annual course of the components of
external heat balance on the sea surface whose climatic anomalies, parallel with the meridional heat and water transfer in
the ocean-atmosphere system, specify the intraannual and interannual large-scale variations of weather in different regions
of the Earth. The development of these studies is connected with the progress of satellite hydrophysics because the data obtained
from the space become sufficiently exact, regular, and global. The increase in the existing data array on the external heat
balance of the oceans from ∼15–20 to 100 yr and more would promote the solution of the problem of oscillations of Earth's
climate. We present examples of coordinated numerical analysis of the heat balance of the upper (0–100 m ) layer of the Black
Sea performed on the basis of the shipborne and satellite data.
__________
Translated from Morskoi Gidrofizicheskii Zhurnal, No. 6, pp. 59–75, November–December, 2007. 相似文献
895.
Isotopic variation of fishes in freshwater and estuarine zones of a large subtropical coastal lagoon
A.M. Garcia D.J. Hoeinghaus J.P. Vieira K.O. Winemiller 《Estuarine, Coastal and Shelf Science》2007,73(3-4):399-408
We used stable C and N isotope ratios of tissues from 29 fish species from a large subtropical lagoon in southern Brazil to examine spatial variability in isotopic composition and vertical trophic structure across freshwater and estuarine habitats. Nitrogen isotope ratios indicated a smooth gradation in trophic positions among species, with most fishes occupying the secondary and tertiary consumer level. Fish assemblages showed a significant shift in their carbon isotopic signatures between freshwater and estuarine sites. Depleted carbon signatures (from −24.7‰ to −17.8‰) were found in freshwater, whereas more enriched signatures (from −19.1‰ to −12.3‰) were obtained within the estuarine zone downstream. Based on our survey of the C3 and C4 plants and isotopic values for phytoplankton and benthic microalgae reported for ecosystems elsewhere, we hypothesized that the observed δ13C differences in the fish assemblage between freshwater and estuarine sites is due to a shift from assimilating organic matter ultimately derived from C3 freshwater marsh vegetation and phytoplankton at the freshwater site (δ13C ranging from −25‰ to −19‰), to C4 salt-marsh (e.g. Spartina) and widgeon grass (Ruppia maritima), benthic microalgae and marine phytoplankton at the estuarine sites (from −18‰ to −12‰). Our results suggested that fish assemblages are generally supported by autochthonous primary production. Freshwater fishes that likely were displaced downstream into the estuary during periods of high freshwater discharge had depleted δ13C values that were characteristic of the upper lagoon. These results suggest that spatial foodweb subsidies can occur within the lagoon. 相似文献
896.
897.
On October 3 and 4, 1986, DSRVAlvin dives encountered a strong current at 2,300 m in South Wilmington Canyon. The current, estimated at 1 knot, transported surficial
sediment and constructed and modified bedforms. It appears to have been constant in its direction of flow from 30 to 40°.
The observed current was probably a burst of fast flow in a region of slow average currents in the Deep Western Boundary Undercurrent.
Such episodic events may have a greater influence on the stratigraphic record than the temporally longer more tranquil flow
conditions. 相似文献
898.
Surface currents influenced by a wind-driven upwelling event in San Pedro Bay moved total suspended matter (TSM) confined
to the inner shelf on 19 April 1978 seaward, so that by 27 April surface TSM had increased over the outer shelf. Near-bottom
concentrations of TSM also increased across the shelf during this time. This is explained by sediment resuspended by large
surface waves being advected from the inner shelf seaward by the mean flow after this flow had turned from southeasterly to
southerly when upwelling ceased on 26 April. These complex shelf dynamics contribute to the off-shelf transport of mud to
the slope and deep basins. 相似文献
899.
Abstract. Anaerobic metabolism in the central and marginal portions of the mantle of Mercenaria mercenaria was compared. Anaerobic succinate accumulation was more rapid in the central region. This difference may be due to higher phosphoenolpyruvate carboxykinase activity in the central region. Thus, the central region is more specialized for anaerobic metabolism and the marginal region more for net shell growth. The original rate of succinate accumulation in the mantle is similar in isolated mantles and intact clams, suggesting that mantle succinate production does not require translocation of precursors from other tissues. However, in intact clams, the rate of succinate accumulation in the central region of the mantle slows after four hours. The reduced rate is probably caused by reducing the metabolic rate. Succinate accumulation and shell dissolution are slower in freshly collected clams than in clams that had been stored anaerobically. The difference may be due to induction of PEPCK synthesis during storage. Shell derived calcium did not accumulate in the mantle and, therefore did not alter the intracellular calcium concentration in the mantle. 相似文献
900.
Louis I. Gordon P. Kilho Park Stephen W. Hager Timothy R. Parsons 《Journal of Oceanography》1971,27(3):81-90
Observations were made of time variations of the carbon dioxide partial pressures (Pco2) of the atmosphere and surface sea waters in the Pacific subarctic region. Data were obtained on a cruise of the USC & GSSSURVEYOR in October, 1968 and on the TRANSPAC expedition of the CNAVENDEAVOUR in March–April, 1969. A rise in surface water Pco2 of 18×10–6 atm occurred in a period of 30–45 days in March–April due principally to spring warming of surface waters. An average increase of 60×10–6 atm occurred between October, 1968 and March, 1969 as a result mainly of cessation of summer phytoplankton production and the onset of winter-storm-driven vertical mixing. Because the air-sea Pco2 gradient not only changed appreciably in magnitude but also changed sign, there are important implications for calculations of air-sea exchange of carbon dioxide on the ocean wide scale.Data contained in this paper comprise part of a dissertation to be submitted by Louis I. Gordon in partial fulfillment of the requirements for the Ph. D. at Oregon State University. 相似文献