全文获取类型
收费全文 | 196篇 |
免费 | 4篇 |
国内免费 | 2篇 |
专业分类
测绘学 | 1篇 |
大气科学 | 28篇 |
地球物理 | 35篇 |
地质学 | 56篇 |
海洋学 | 7篇 |
天文学 | 61篇 |
自然地理 | 14篇 |
出版年
2022年 | 2篇 |
2021年 | 7篇 |
2020年 | 3篇 |
2019年 | 4篇 |
2018年 | 3篇 |
2017年 | 4篇 |
2016年 | 7篇 |
2015年 | 8篇 |
2014年 | 7篇 |
2013年 | 15篇 |
2012年 | 5篇 |
2011年 | 6篇 |
2010年 | 6篇 |
2009年 | 8篇 |
2008年 | 7篇 |
2007年 | 5篇 |
2006年 | 6篇 |
2005年 | 4篇 |
2004年 | 4篇 |
2003年 | 4篇 |
2002年 | 2篇 |
2001年 | 5篇 |
2000年 | 4篇 |
1999年 | 5篇 |
1997年 | 5篇 |
1996年 | 4篇 |
1994年 | 3篇 |
1991年 | 4篇 |
1989年 | 6篇 |
1988年 | 2篇 |
1985年 | 3篇 |
1984年 | 2篇 |
1983年 | 3篇 |
1980年 | 2篇 |
1979年 | 3篇 |
1978年 | 3篇 |
1977年 | 4篇 |
1976年 | 3篇 |
1975年 | 2篇 |
1974年 | 3篇 |
1973年 | 1篇 |
1971年 | 1篇 |
1960年 | 3篇 |
1958年 | 1篇 |
1957年 | 1篇 |
1956年 | 2篇 |
1954年 | 1篇 |
1953年 | 1篇 |
1952年 | 1篇 |
1942年 | 1篇 |
排序方式: 共有202条查询结果,搜索用时 31 毫秒
41.
Joseph D. Conroy Leon Boegman Hongyan Zhang William J. Edwards David A. Culver 《Aquatic Sciences - Research Across Boundaries》2011,73(2):289-304
Calculated hypolimnetic oxygen depletion (HOD) rates depend not only on environmental factors but also logistical ones. In
particular, lack of understanding of the effects of weather in addition to how sampling effort determines calculated HOD rates
complicates ecological understanding and environmental management of lake ecosystems. To better determine the roles of weather
and sampling effort, we combined (1) weekly measurements of temperature and dissolved oxygen (DO) concentrations from seven
stations in the Sandusky subbasin of Lake Erie’s central basin during 2005, (2) contemporaneous measures of storm activity
and tributary discharge, and (3) a two-dimensional coupled hydrodynamic, chemical, and biological model of Lake Erie to investigate
(1) how increased storm activity and tributary discharge affected short- (daily) and long-term (seasonal) dynamics of hypolimnetic
hypoxia, and (2) how spatial (number of sites sampled) and temporal (sampling frequency) sampling effort affected calculated
HOD rates. Our model closely replicated field-observed DO dynamics. When comparing baseline modeled dynamics to those in a
second simulation with twice the number of days with high winds, however, we found that with more storm activity (1) periods
of entrainment became more frequent, (2) the hypolimnion was warmer, (3) thermal stratification occurred 1 month later, whereas
autumnal turnover occurred at least 1 week earlier shortening the duration of stratification by 1–2 months, and (4) HOD rates
increased 12%. Further, spatial and temporal sampling intensity also affected calculated HOD rates. Consequently, adequately
quantifying actual HOD rates requires sufficient sampling effort and the particular role of weather should be assessed with
rigorous field and simulation studies, especially if HOD rates are used to indicate management success. 相似文献
42.
Geological and thermochronological studies of the Dashui gold deposit, West Qinling Orogen, Central China 总被引:3,自引:0,他引:3
Qingtao Zeng Noreen J. Evans Brent I. A. McInnes Geoffrey E. Batt Campbell T. McCuaig Leon Bagas Eric Tohver 《Mineralium Deposita》2013,48(3):397-412
The Dashui gold deposit is a structurally controlled, Carlin-type gold deposit hosted by recrystallised limestone in the West Qinling Orogen of Central China. The major, structurally late east-trending Dashui Fault forms the hanging wall to the gold mineralisation at the Dashui mine and defines the contact between Middle Triassic limestone and a steeply dipping overlying succession of Middle Triassic argillaceous limestone, dolomite, and sandstone. Multiple carbonate veins and large-scale supergene enrichment, represented by hematite, goethite, limonite and jarosite, characterise the deposit. Detailed geochronological investigation using zircon SHRIMP U-Pb dating reveals that volcanic rocks closely associated with the Dashui gold deposit were synchronous with the Ge’erkuohe Granite and pre-date mineralisation. The igneous dyke sample from the hanging wall has the same U-Pb zircon age as the footwall, ca. 213 Ma. (U-Th)/He thermochronology on dykes in the hanging wall and footwall of the Dashui Fault yields identical (U-Th)/He zircon ages of ca. 210 Ma but distinct (U-Th)/He apatite ages of ca. 136 and 211 Ma, respectively. Therefore, the hanging wall and footwall are interpreted as having distinct post-mineralisation exhumation histories. Reverse fault movement exhumed the hanging wall ~2 to 4 km since the Late Triassic with the main component of faulting taking place between the Late Triassic and Early Cretaceous. These relationships suggest a Late Triassic to Early Cretaceous age for the primary gold mineralisation at the Dashui gold deposit, with the corollary that any ‘missing portion’ of the deposit, previously hypothesised to exist in the hanging wall of the Dashui Fault, has been eroded away. The mineralisation in the footwall may have been supergene enriched soon after the primary mineralisation was emplaced, because it has been located at shallow depth since the Late Triassic. Semi-quantitative results obtained in this study also constrain the maximum depth of formation of the Dashui gold at no more than 2 km. 相似文献
43.
44.
Glauconite from eight stratigraphic horizons (Cambrian to Pennsylvanian) in the Llano Uplift, central Texas and two Cretaceous glauconites were analyzed by the Rb-Sr method. Only two untreated samples provide ages in agreement with those anticipated from current best estimates of the geologic time scale. With one exception all the other apparent ages fall short of the estimated age of deposition by as much as 22%. Low ages, the pattern customarily observed, are attributed to postdepositional loss of radiogenic 87Sr from expandable layers by weathering or during diagenesis.Detailed leaching experiments using a variety of reagents were performed to characterize the behavior of glauconite. The most promising treatment, which we recommend as standard procedure in all future studies, is with ammonium acetate which is able to purge the mineral of loosely-bound Rb and Sr while leaving tightly-bound components intact. After appropriate leach, three other Rb-Sr ages were brought into coincidence with their estimated ages of deposition.In contrast an Upper Cambrian glauconite was found to be extremely resistant to further alteration by chemical attack′, providing an age of 429 ± 17 M yr. Although 17% short of the age of deposition, this age is interpreted as the time of a real event: diagenetic recrystallization induced by burial. Comparison of data from four samples indicates that for Paleozoic glauconite, conditions exist in which the Rb-Sr system is less susceptible to mild disturbance than is the K-Ar system. 相似文献
45.
Fracture set properties such as orientation, spacing, trace length, and waviness tend to be spatially correlated. These properties can be efficiently simulated by spectral analysis procedures that take advantage of the computational speed of the fast Fourier transform. The covariance function of each property to be simulated is obtained from the variogram function estimated from mapped fracture set data and is typically referenced to the mean vector of the set. Simulation procedures for normally and exponentially distributed data involve generating uncorrelated Fourier coefficients that are assigned proper variance according to the spectral density, which is the Fourier transform of the covariance function. These coefficients are then reverse Fourier transformed to produce simulated set properties that have the desired variance and variogram function. 相似文献
46.
L. Golub 《Astrophysics and Space Science》1996,237(1-2):33-48
The solar corona, and the coronae of solar-type stars, consist of a low-density magnetized plasma at temperatures exceeding
106 K. The primary coronal emission is therefore in the UV and soft x-ray range. The observed close connection between solar
magnetic fields and the physical parameters of the corona implies a fundamental role for the magnetic field in coronal structuring
and dynamics. Variability of the corona occurs on all temporal and spatial scales—at one extreme, as the result of plasma
instabilities, and at the other extreme driven by the global magnetic flux emergence patterns of the solar cycle. 相似文献
47.
Katherine?CalvinEmail author Marshall?Wise Patrick?Luckow Page?Kyle Leon?Clarke Jae?Edmonds 《Climatic change》2016,136(1):57-68
The magnitude and character of the global resource base of fossil fuels is a key determinant of the evolution of the future global energy system and corresponding fossil fuel carbon emissions. What is less well understood is the potential magnitude of impact of the availability of fossil fuels, due to the interaction with biomass energy, on agriculture, land use, ecosystems and therefore carbon emissions from land-use change. This paper explores these links and implications. We show that if oil resources are limited, then the consequently higher price for liquids induces both the use of coal-to-liquids technology deployment, but also enhanced production of bioenergy crops particularly in a business-as-usual scenario. This in turn implies greater pressure to convert unmanaged ecosystems to produce bioenergy, and higher rates of terrestrial carbon emissions from land use. 相似文献
48.
Cathyrn A. Manduca Leon T. Silver Hugh P. Taylor 《Contributions to Mineralogy and Petrology》1992,109(3):355-372
A spatially abrupt geochemical boundary is preserved within four plutonic complexes along the western margin of the Cretaceous Idaho Batholith near McCall, Idaho. These intrusives ranging in composition from tonalite to granite were emplaced across a regional boundary between accreted oceanic-arc terranes and the continental margin, and their isotopic, major-element, and trace-element geochemistry provide detailed information about this change in crustal characteristics at depth, indicating that the boundary is nearly vertical and extends deep into the lithosphere. The Hazard Creek complex, emplaced west of the transition in wall-rock lithology, has initial 87Sr/86Sr (Ri) less than 0.7045 and 18O greater than 7.5, indicating little or no continental crust in its source region; however, elevated 18O requires some incorporation of rocks formed or altered at the earth's surface. A large shift in Ri and 18O is observed across the 5–8 km wide Little Goose Creek complex, which was emplaced across the wall-rock boundary. This is interpreted as mixing between: (1) a basaltic or andesitic magma with low K2O and high Na2O, Al2O3, and Sr, similar to that forming the Hazard Creek complex; and (2) materials similar to Precambrian sedimentary sedimentary rocks with low Sr, high 18O (+15) and high Ri (0.83 at 100 Ma). The Payette River complex, emplaced east of the wall-rock boundary, exhibits at least one additional component with low 18O (+6), moderate Ri (0.708) and mafic composition. This component is inferred to be old basaltic material in the lower crust or upper mantle similar to that inferred to be a minor part of the Peninsular Ranges Batholith in SE California (Silver et al. 1979; Hill et al. 1986). The easternmost complex in the Idaho transect is made up of granites that may contain a component of granitic cratonal basement. The entire west-to-east geochemical transition from oceanic-arc magmas to cratonal magmas takes place over a lateral distance of less than 20 km. Although the zone of transitional protolith dominated by metasedimentary rocks is unusually narrow and may have been in part tectonically removed, the striking geochemical similarities between this traverse and several other transects across much broader areas of Nevada and California suggest that the craton itself was not rifted apart, but that juxtaposition of the accreted oceanic-arc terranes occurred along the preexisting craton margin. The data confirm that the isotopic geochemistry of granitoid plutons can be used as a probe of deep lithospheric character, and that major lateral variations in the lithosphere on the order of one to two kilometers in width can be recognized in favorable circumstances. 相似文献
49.
50.
Hang Lei Gao YuFeng He Jia Li Chi Zhou YunDong van Paassen Leon A. 《Acta Geotechnica》2022,17(12):5429-5439
Acta Geotechnica - In the biocement–geosynthetic system, biocement is combined with geosynthetic to increase the pullout resistance of the geosynthetic and thereby the stability of reinforced... 相似文献