全文获取类型
收费全文 | 400篇 |
免费 | 15篇 |
国内免费 | 3篇 |
专业分类
测绘学 | 8篇 |
大气科学 | 34篇 |
地球物理 | 97篇 |
地质学 | 112篇 |
海洋学 | 24篇 |
天文学 | 105篇 |
自然地理 | 38篇 |
出版年
2022年 | 2篇 |
2021年 | 4篇 |
2020年 | 9篇 |
2019年 | 8篇 |
2018年 | 11篇 |
2017年 | 14篇 |
2016年 | 15篇 |
2015年 | 14篇 |
2014年 | 12篇 |
2013年 | 21篇 |
2012年 | 4篇 |
2011年 | 15篇 |
2010年 | 14篇 |
2009年 | 22篇 |
2008年 | 37篇 |
2007年 | 27篇 |
2006年 | 23篇 |
2005年 | 16篇 |
2004年 | 18篇 |
2003年 | 22篇 |
2002年 | 6篇 |
2001年 | 8篇 |
2000年 | 6篇 |
1999年 | 5篇 |
1998年 | 5篇 |
1996年 | 4篇 |
1995年 | 7篇 |
1994年 | 5篇 |
1993年 | 2篇 |
1992年 | 3篇 |
1991年 | 4篇 |
1990年 | 5篇 |
1989年 | 2篇 |
1988年 | 2篇 |
1987年 | 2篇 |
1986年 | 3篇 |
1985年 | 7篇 |
1984年 | 4篇 |
1981年 | 4篇 |
1980年 | 3篇 |
1979年 | 1篇 |
1978年 | 3篇 |
1977年 | 1篇 |
1976年 | 3篇 |
1974年 | 3篇 |
1973年 | 3篇 |
1972年 | 2篇 |
1968年 | 1篇 |
1967年 | 2篇 |
1966年 | 1篇 |
排序方式: 共有418条查询结果,搜索用时 15 毫秒
71.
Yves Moussallam Clive Oppenheimer Alessandro Aiuppa Gaetano Giudice Manuel Moussallam Philip Kyle 《Bulletin of Volcanology》2012,74(9):2109-2120
The continuous measurement of molecular hydrogen (H2) emissions from passively degassing volcanoes has recently been made possible using a new generation of low-cost electrochemical sensors. We have used such sensors to measure H2, along with SO2, H2O and CO2, in the gas and aerosol plume emitted from the phonolite lava lake at Erebus volcano, Antarctica. The measurements were made at the crater rim between December 2010 and January 2011. Combined with measurements of the long-term SO2 emission rate for Erebus, they indicate a characteristic H2 flux of 0.03?kg s–1 (2.8?Mg? day–1). The observed H2 content in the plume is consistent with previous estimates of redox conditions in the lava lake inferred from mineral compositions and the observed CO2/CO ratio in the gas plume (~0.9 log units below the quartz–fayalite–magnetite buffer). These measurements suggest that H2 does not combust at the surface of the lake, and that H2 is kinetically inert in the gas/aerosol plume, retaining the signature of the high-temperature chemical equilibrium reached in the lava lake. We also observe a cyclical variation in the H2/SO2 ratio with a period of ~10?min. These cycles correspond to oscillatory patterns of surface motion of the lava lake that have been interpreted as signs of a pulsatory magma supply at the top of the magmatic conduit. 相似文献
72.
Kyle McMillan 《Journal of Paleolimnology》2008,40(4):1179-1184
Representative images of split sediment cores document geological records, serve as visual aids for multimedia, and provide
samples for image analysis. Existing core imaging systems, often containing integrated hardware and software, are capable
of providing excellent images; unfortunately these systems are also bulky and expensive, and are therefore limited to labs
that process large volumes of core and those actively involved in image analysis. For most research groups such systems are
unfeasible to buy and maintain. Producing good quality core images with a hand-held digital camera is very difficult without
a consistent lighting source, and changes in camera angle (in all three spatial dimensions) between photographs may prevent
accurate image compositing. Tripods allow for camera stability, but typically do not accommodate downward-facing photography.
Presented here is an easily constructed core-imaging system that minimizes many of the drawbacks of personal digital cameras.
Software necessary for using this system is readily available and can be run from a personal computer. 相似文献
73.
Malinda L. Kent‐Corson Andreas Mulch Stephan A. Graham Alan R. Carroll Bradley D. Ritts C. Page Chamberlain 《Basin Research》2010,22(6):829-845
Early Cenozoic terrestrial deposits in the western United States represent well‐preserved archives of climatic and tectonic processes that together shaped the Earth's surface during the demise of a large continental plateau. This study examines a Cenozoic terrestrial sedimentary sequence in the central part of the Cordilleran orogen (Montana) using sedimentologic and geochemical techniques. At ~49 Ma, we observe rapid major shifts in oxygen, carbon and strontium isotope records that are too large to directly reflect changes in meteoric water composition due to simple orographic rainout. The transition to low‐δ18O values in pedogenic carbonate in concert with changes in the composition of clastic material at ~49 Ma points to the input of evolved meteoric water to the hydrological cycle due to a change in the source of waters reaching Cordilleran intermontane regions in southwestern Montana. This drainage reorganization coincides with the initiation of magmatism and extension to the west in what is now Montana and Idaho. The sedimentological record shows evidence that depositional gradients increased in the study area ~46 Ma, ~3 Myr after the drainage reorganization occurred. This interval is most likely the time it took for extensional deformation to propagate to the study area itself. Evidence of freshening events in Laramide Basins to the southeast suggests that this drainage reorganization diverted waters to progressively fill these basins and highlights the impact of post‐plateau extension‐related landscape reorganization on river networks and lake dynamics. This study also emphasizes the importance of using multiple tools in deciphering topographic history through the study of terrestrial basin deposits, in that interpretation based on any single method employed would have compromised our ability to successfully identify the regional evolution of topography and drainage networks. 相似文献
74.
75.
M. A. Page 《地球物理与天体物理流体动力学》2013,107(1-2):51-69
Abstract The low Rossby number flow in a rotating cylinder with an inclined bottom, of small slope, is examined when part of the lid of the container is rotating at a slightly different rate. The resulting flow is calculated numerically by solving the governing equations for the two-dimensional geostrophic motion which approximates the flow in most of the fluid including the inertially-modified E ¼ -layers. The presence of ageostrophic regions, on the container walls and beneath the velocity discontinuity on the lid, is accounted for in the governing equations and their boundary conditions. This study supplements previous work on this configuration, in which the zero Rossby number flow was calculated and experimental results were presented, by enabling a direct comparison to be made between the results of the low Rossby number theory and the experiments. The numerical results for a range of Rossby and Ekman numbers compare well with those from the experiments despite a severe limitation on the size of the Rossby number arising from the analysis in the ageostrophic part of the detached shear layer. 相似文献
76.
77.
A Kalman filter-based method combining the energy of both L1 C/A and L2C GPS signals in a combined tracking loop method to
enhance performance under adverse conditions is developed. Standard tracking methods and the ionospheric effect on GPS signals
are reviewed and compared to a new Kalman filter that simultaneously estimates delay, phase and total electron content by
combining L1 C/A and L2C code and phase discriminator outputs. The new filter is tested and compared to standard methods for
tracking L1 C/A and L2C using both simulated and real data. The new method is found to have improved sensitivity of 3 dB compared
to standard L1 tracking and 4.5 dB compared to standard L2C tracking while at the same time providing an accurate estimate
of the total electron content along the signal path. 相似文献
78.
Jenifer E. Dugan David M. Hubbard Henry M. Page Joshua P. Schimel 《Estuaries and Coasts》2011,34(4):839-850
We investigated the role of sandy beaches in nearshore nutrient cycling by quantifying macrophyte wrack inputs and examining
relationships between wrack accumulation and pore water nutrients during the summer dry season. Macrophyte inputs, primarily
giant kelp Macrocystis pyrifera, exceeded 2.3 kg m−1 day−1. Mean wrack biomass varied 100-fold among beaches (range = 0.41 to 46.43 kg m−1). Mean concentrations of dissolved inorganic nitrogen (DIN), primarily NOx−-N, and dissolved organic nitrogen (DON) in intertidal pore water varied significantly among beaches (ranges = 1 to 6,553 μM
and 7 to 2,006 μM, respectively). Intertidal DIN and DON concentrations were significantly correlated with wrack biomass.
Surf zone concentrations of DIN were also strongly correlated with wrack biomass and with intertidal DIN, suggesting export
of nutrients from re-mineralized wrack. Our results suggest beach ecosystems can process and re-mineralize substantial organic
inputs and accumulate dissolved nutrients, which are subsequently available to nearshore waters and primary producers. 相似文献
79.
Kyle M. Straub David MohrigJames Buttles Brandon McElroyCarlos Pirmez 《Marine and Petroleum Geology》2011,28(3):744-760
Here we present results from a suite of laboratory experiments that highlight the influence of channel sinuosity on the depositional mechanics of channelized turbidity currents. We released turbidity currents into three channels in an experimental basin filled with water and monitored current properties and the evolution of topography via sedimentation. The three channels were similar in cross-sectional geometry but varied in sinuosity. Results from these experiments are used to constrain the run-up of channelized turbidity currents on the outer banks of moderate to high curvature channel bends. We find that a current is unlikely to remain contained within a channel when the kinetic energy of a flow exceeds the potential energy associated with an elevation gain equal to the channel relief; setting an effective upper limit for current velocity. Next we show that flow through bends induces a vertical mixing that redistributes suspended sediment back into the interiors of depositional turbidity currents. This mixing counteracts the natural tendency for suspended sediment concentration and grain size to stratify vertically, thereby reducing the rate at which sediment is lost from a current via deposition. Finally, the laboratory experiments suggest that turbidity currents might commonly separate from channel sidewalls along the inner banks of bends. In some cases, sedimentation rates and patterns within the resulting separation zones are sufficient to construct bar forms that are attached to the channel sidewalls and represent an important mechanism of submarine channel filling. These bar forms have inclined strata that might be mistaken for the deposits of point bars and internal levees, even though the formation mechanism and its implications to channel history are different. 相似文献
80.
Peter J. Kelly Nelia W. Dunbar Philip R. Kyle William C. McIntosh 《Journal of Volcanology and Geothermal Research》2008
Six new 40Ar/39Ar and three cosmogenic 36Cl age determinations provide new insight into the late Quaternary eruptive history of Erebus volcano. Anorthoclase from 3 lava flows on the caldera rim have 40Ar/39Ar ages of 23 ± 12, 81 ± 3 and 172 ± 10 ka (all uncertainties 2σ). The ages confirm the presence of a second, younger, superimposed caldera near the southwestern margin of the summit plateau and show that eruptive activity has occurred in the summit region for 77 ± 13 ka longer than previously thought. Trachyte from “Ice Station” on the eastern flank is 159 ± 2 ka, similar in age to those at Bomb Peak and Aurora Cliffs. The widespread occurrences of trachyte on the eastern flank of Erebus suggest a major previously unrecognized episode of trachytic volcanism. The trachyte lavas are chemically and isotopically distinct from alkaline lavas erupted contemporaneously in the summit region < 5 km away. 相似文献