全文获取类型
收费全文 | 851篇 |
免费 | 60篇 |
国内免费 | 9篇 |
专业分类
测绘学 | 53篇 |
大气科学 | 65篇 |
地球物理 | 213篇 |
地质学 | 288篇 |
海洋学 | 81篇 |
天文学 | 131篇 |
综合类 | 6篇 |
自然地理 | 83篇 |
出版年
2023年 | 4篇 |
2022年 | 6篇 |
2021年 | 28篇 |
2020年 | 12篇 |
2019年 | 19篇 |
2018年 | 34篇 |
2017年 | 35篇 |
2016年 | 49篇 |
2015年 | 31篇 |
2014年 | 27篇 |
2013年 | 57篇 |
2012年 | 42篇 |
2011年 | 45篇 |
2010年 | 42篇 |
2009年 | 58篇 |
2008年 | 44篇 |
2007年 | 44篇 |
2006年 | 37篇 |
2005年 | 22篇 |
2004年 | 42篇 |
2003年 | 29篇 |
2002年 | 21篇 |
2001年 | 19篇 |
2000年 | 28篇 |
1999年 | 14篇 |
1998年 | 12篇 |
1997年 | 8篇 |
1996年 | 11篇 |
1995年 | 6篇 |
1994年 | 3篇 |
1993年 | 7篇 |
1991年 | 8篇 |
1990年 | 5篇 |
1988年 | 4篇 |
1987年 | 2篇 |
1986年 | 3篇 |
1984年 | 6篇 |
1983年 | 12篇 |
1982年 | 6篇 |
1981年 | 5篇 |
1980年 | 3篇 |
1979年 | 3篇 |
1978年 | 3篇 |
1977年 | 4篇 |
1976年 | 4篇 |
1975年 | 2篇 |
1974年 | 5篇 |
1973年 | 2篇 |
1972年 | 2篇 |
1967年 | 1篇 |
排序方式: 共有920条查询结果,搜索用时 16 毫秒
851.
Tom Bradwell 《Geografiska Annaler: Series A, Physical Geography》2004,86(1):31-41
Abstract The age of recent deposits can be determined using an intrinsic characteristic of the lichen ‘population’ growing on their surface. This paper presents a calibrated dating curve based on the gradient of the size‐frequency distribution of yellow‐green Rhizocarpon lichens. The dating potential of this new curve is tested on surfaces of known age in southeast Iceland. This particular size—frequency technique is also compared with the more traditional largest‐lichen approach. The results are very encouraging and suggest that the gradient can be used as an age indicator, at least on deposits formed within the last c. 150 years – and probably within the last c. 400 years – in the maritime subpolar climate of southeast Iceland. Using both lichenometric techniques, revised dates for moraines on two glacier forelands are presented which shed new light on the exact timing of the Little Ice Age glacier maximum in Iceland. 相似文献
852.
Maria Luce Frezzotti Tom Andersen Else-Ragnhild Neumann Siri Lene Simonsen 《Lithos》2002,64(3-4):77-96
Three types of fluid inclusions have been identified in olivine porphyroclasts in the spinel harzburgite and lherzolite xenoliths from Tenerife: pure CO2 (Type A); carbonate-rich CO2–SO2 mixtures (Type B); and polyphase inclusions dominated by silicate glass±fluid±sp±silicate±sulfide±carbonate (Type C). Type A inclusions commonly exhibit a “coating” (a few microns thick) consisting of an aggregate of a platy, hydrous Mg–Fe–Si phase, most likely talc, together with very small amounts of halite, dolomite and other phases. Larger crystals (e.g. (Na,K)Cl, dolomite, spinel, sulfide and phlogopite) may be found on either side of the “coating”, towards the wall of the host mineral or towards the inclusion center. These different fluids were formed through the immiscible separations and fluid–wall-rock reactions from a common, volatile-rich, siliceous, alkaline carbonatite melt infiltrating the upper mantle beneath the Tenerife. First, the original siliceous carbonatite melt is separated from a mixed CO2–H2O–NaCl fluid and a silicate/silicocarbonatite melt (preserved in Type A inclusions). The reaction of the carbonaceous silicate melt with the wall-rock minerals gave rise to large poikilitic orthopyroxene and clinopyroxene grains, and smaller neoblasts. During the metasomatic processes, the consumption of the silicate part of the melt produced carbonate-enriched Type B CO2–SO2 fluids which were trapped in exsolved orthopyroxene porphyroclasts. At the later stages, the interstitial silicate/silicocarbonatite fluids were trapped as Type C inclusions. At a temperature above 650 °C, the mixed CO2–H2O–NaCl fluid inside the Type A inclusions were separated into CO2-rich fluid and H2O–NaCl brine. At T<650 °C, the residual silicate melt reacted with the host olivine, forming a reaction rim or “coating” along the inclusion walls consisting of talc (or possibly serpentine) together with minute crystals of NaCl, KCl, carbonates and sulfides, leaving a residual CO2 fluid. The homogenization temperatures of +2 to +25 °C obtained from the Type A CO2 inclusions reflect the densities of the residual CO2 after its reactions with the olivine host, and are unrelated to the initial fluid density or the external pressure at the time of trapping. The latter are restricted by the estimated crystallization temperatures of 1000–1200 °C, and the spinel lherzolite phase assemblage of the xenolith, which is 0.7–1.7 GPa. 相似文献
853.
Glen R. Walker Lu Zhang Tim W. Ellis Tom J. Hatton Cuan Petheram 《Hydrogeology Journal》2002,10(1):68-90
To manage dryland salinity, one needs to know how changed land use affects groundwater recharge. Few techniques are available
for comparing 'deep drainage' under different land uses. Soil-tracer methods, although good for replication and remote field
sites, are subject to spatial variability. Lysimeters are good for comparisons but are difficult for drier areas and sloping
land. Agronomic water-balance studies, where appropriate soil-water measurements exist, may be used with a soil-vegetation
model to estimate long-term deep drainage. Complex models are required to analyze specific land-use differences, such as perenniality
and root and leaf area dynamics, but models require intensive and extensive data for calibration. This approach is time-consuming,
labour-intensive, and difficult in remote locations. Because of the one-dimensionality of most soil-vegetation models and
the small fraction of the total water balance that is deep drainage, little success has occurred in extrapolating beyond the
research plot, or to spatially heterogeneous systems such as alley farming. Some 'top-down' modelling and landscape disaggregation
approaches have been partially successful in making catchment or regional-scale predictions. The direction for further work
depends on the level of recharge reduction that is required for most groundwater systems and difficulties that it imposes.
Electronic Publication 相似文献
854.
With the advances in the field of GPS positioning and the global densification of permanent GPS tracking stations, it is now
possible to determine at the highest level of accuracy the transformation parameters connecting various international terrestrial
reference frame (ITRF) realizations. As a by-product of these refinements, not only the seven usual parameters of the similarity
transformations between frames are available, but also their rates, all given at some epoch t
k
. This paper introduces rigorous matrix equations to estimate variance–covariance matrices for transformed coordinates at
any epoch t based on a stochastic model that takes into consideration all a priori information of the parameters involved at epoch t
k
, and the coordinates and velocities at the reference frame initial epoch t
0. The results of this investigation suggest that in order to attain maximum accuracy, the agencies determining the 14-parameter
transformations between reference frames should also publish their full variance–covariance matrix.
Electronic Publication 相似文献
855.
A comparison between the variation trend of alkaline basaltic magmas within the CaO-MgO-Al2O3-SiO2 system and experimentally estimated phase relations for this system at high pressures, suggests an olivine reaction relationship, which may explain the transition from primary magmas in equilibrium with olivine to alkaline basaltic magmas in which olivine does not form at high pressures. This reaction relationship is considered to be due to a transition from positive to negative crystallization with respect to olivine along the four phase curve where olivine, diopside, pyrope garnet and liquid are initially in equilibrium. The bimineralic, eclogitic character of alkaline basaltic compositions at high pressures is interpreted as being due to the presence of a thermal minimum on the three phase surface, where dioside and pyrope garnet are in equilibrium with liquid. 相似文献
856.
The content of FeS in sphalerites from different parts of a boudinage is compared with the theoretical stress pattern. The calculated differences in stress correspond to less than one mole percent FeS and are often masked by the small variations in the fugacity of sulfur. 相似文献
857.
858.
Tom Beer 《Planetary and Space Science》1978,26(2):185-188
The dominant response of the terminator is found to be due to the change in thermospheric absorption of solar radiation, and leads to two types of atmospheric waves: (i) a ducted acoustic wave at altitudes below 100 km and (ii) a boundary wave concentrated along the mesopause. 相似文献
859.
860.
Large‐scale streamlined glacial landforms are identified in 11 areas of northwest Scotland, from the Isle of Skye in the south to the Butt of Lewis in the north. These ice‐directional features occur in bedrock and superficial deposits, generally below 350 m above sea level, and where best developed have elongation ratios of >20:1. Sidescan sonar and multibeam echo‐sounding data from The Minch show elongate streamlined ridges and grooves on the seabed, with elongation ratios of up to 70:1. These bedforms are interpreted as mega‐scale glacial lineations. All the features identified formed beneath The Minch palaeo‐ice stream which was ca. 200 km long, up to 50 km wide and drained ca. 15 000 km2 of the northwest sector of the last British‐Irish Ice Sheet (Late Devensian Glaciation). Nine ice‐stream tributaries and palaeo‐onset zones are also identified, on the basis of geomorphological evidence. The spatial distribution and pattern of streamlined bedforms around The Minch has enabled the catchment, flow paths and basal shear stresses of the palaeo‐ice stream and its tributaries to be tentatively reconstructed. © British Geological Survey/Natural Environment Research Council copyright 2007. Reproduced with the permission of BGS/NERC. Published by John Wiley & Sons, Ltd. 相似文献