全文获取类型
收费全文 | 926篇 |
免费 | 64篇 |
国内免费 | 2篇 |
专业分类
测绘学 | 30篇 |
大气科学 | 45篇 |
地球物理 | 344篇 |
地质学 | 330篇 |
海洋学 | 20篇 |
天文学 | 156篇 |
综合类 | 13篇 |
自然地理 | 54篇 |
出版年
2023年 | 6篇 |
2022年 | 10篇 |
2021年 | 13篇 |
2020年 | 17篇 |
2019年 | 18篇 |
2018年 | 58篇 |
2017年 | 58篇 |
2016年 | 77篇 |
2015年 | 64篇 |
2014年 | 61篇 |
2013年 | 64篇 |
2012年 | 46篇 |
2011年 | 38篇 |
2010年 | 39篇 |
2009年 | 50篇 |
2008年 | 37篇 |
2007年 | 36篇 |
2006年 | 30篇 |
2005年 | 21篇 |
2004年 | 10篇 |
2003年 | 11篇 |
2002年 | 17篇 |
2001年 | 8篇 |
2000年 | 11篇 |
1999年 | 11篇 |
1998年 | 13篇 |
1997年 | 4篇 |
1996年 | 16篇 |
1995年 | 8篇 |
1994年 | 8篇 |
1993年 | 6篇 |
1992年 | 7篇 |
1991年 | 8篇 |
1990年 | 7篇 |
1989年 | 7篇 |
1988年 | 7篇 |
1987年 | 7篇 |
1986年 | 9篇 |
1985年 | 5篇 |
1984年 | 5篇 |
1983年 | 5篇 |
1982年 | 5篇 |
1981年 | 4篇 |
1978年 | 4篇 |
1977年 | 4篇 |
1976年 | 6篇 |
1974年 | 3篇 |
1973年 | 5篇 |
1971年 | 3篇 |
1970年 | 3篇 |
排序方式: 共有992条查询结果,搜索用时 791 毫秒
211.
Wojciech Zgłobicki 《Environmental Earth Sciences》2013,70(7):3085-3092
The geochemical record of human impact within three archaeological sites in SE Poland was analysed. The total levels of Cd, Cu, Pb, Zn and P were defined. The content of the studied elements was found to be higher than the determined geochemical background. In all cases, significantly higher concentrations (2–3 times) of trace metals were found in sediments filling small depressions and foot-slope locations. These concentrations were often higher than in the profiles within the archaeological objects. The vertical distributions of elements were also different from soil profiles located on flat surfaces. The study thus confirms that microtopography and soil erosion may impact (diversify) the initial horizontal and vertical variation of geochemistry of soils within archaeological sites caused by human activity. This should be taken into account when using geochemical prospecting in archaeological studies in areas with varied topography. 相似文献
212.
Lech Krysiński 《Pure and Applied Geophysics》2009,166(3):375-408
The paper describes a new method of gravity modelling of the density cross section along a DSS profile. We propose a systematic
procedure of gravity interpretation using structural information contained both in the velocity distribution of the seismic
model and the geometry of its layers. The procedure is based on the optimisation of the density parameters of the model. The
values of the parameters are limited by relationships between the seismic velocity and the density (optimisation with inequalities).
The formulation of the method allows for discussion of the presence of isostasy and the distribution of compensating masses.
The discussion is very important for the considered crust-lithosphere system. The presented calculations are done for one
Carpathian profile (CEL01). The analysis of the properties of the fitting procedure provides the characteristic depth of subcrustal
compensating density structures, the position of crucial tectonic boundaries along the profiles, locations of the crustal
areas having exceptional lithology, the regional density differences of subcrustal matter and the estimation of regional deviations
from the isostatic equilibrium. 相似文献
213.
Numerical experiments suggest that the last glaciation severely affected the upper lithosphere groundwater system in NW Poland: primarily its flow pattern, velocities and fluxes. We have simulated subglacial groundwater flow in two and three spatial dimensions using finite difference codes for steady‐state and transient conditions. The results show how profoundly the ice sheet modifies groundwater pressure heads beneath and some distance beyond the ice margin. All model runs show water discharge at the ice forefield driven by ice‐sheet‐thickness‐modulated, down‐ice‐decreasing hydraulic heads. In relation to non‐glacial times, the transient 3D model shows significant changes in the groundwater flow directions in a regionally extensive aquifer ca. 90 m below the ice–bed interface and up to 40 km in front of the glacier. Comparison with empirical data suggests that, depending on the model run, only between 5 and 24% of the meltwater formed at the ice sole drained through the bed as groundwater. This is consistent with field observations documenting abundant occurrence of tunnel valleys, indicating that the remaining portion of basal meltwater was evacuated through a channelized subglacial drainage system. Groundwater flow simulation suggests that in areas of very low hydraulic conductivity and adverse subglacial slopes water ponding at the ice sole was likely. In these areas the relief shows distinct palaeo‐ice lobes, indicating fast ice flow, possibly triggered by the undrained water at the ice–bed interface. Owing to the abundance of low‐permeability strata in the bed, the simulated groundwater flow depth is less than ca. 200 m. Copyright © 2009 John Wiley & Sons, Ltd. 相似文献
214.
Comparison of source parameters estimated in the frequency and time domains for seismic events at the Rudna copper mine,Poland 总被引:3,自引:0,他引:3
Source parameters estimated in the frequency domain for 100 selected seismic events from the Rudna copper mine, with moment
magnitude ranging from 1.4 to 3.6, were collected to study their scaling relations and to compare them with the parameters
estimated in the time domain. The apparent stress and static stress drop, corrected for the limited bandwidth recording, increase
slightly in a similar manner with increasing seismic moment. The ratio of apparent stress to static stress drop, a measure
of radiation efficiency, is practically constant and its mean value is close to 0.1.
For 37 seismic events, with moment magnitude between 1.9 and 3.4, source parameters were estimated in the time domain from
relative source time functions, that displayed unilateral rupture propagation, and their rupture velocity could be estimated.
It ranges from 0.23 to 0.80 of shear wave velocity and is almost independent of seismic moment. The fault length, estimated
from the average source pulse width and rupture velocity, is clearly dependent on seismic moment and is smaller than the source
radius estimated from the corner frequency on the average by about 25 percent. There is no correlation between the values
of static stress drop estimated in the frequency and time domains, but the time domain stress drop is in general similar to
that estimated in the frequency domain. The apparent stress increases with increasing rupture velocity, and the ratio of apparent
stress to static stress drop seems also to depend on rupture velocity. 相似文献
215.
216.
Sławomir Maj 《Acta Geophysica》2008,56(4):994-999
The virtual or effective thermal conductivity (ETC) of the Indian subcontinental crust model is calculated from geochemical/geothermal
data on the mean radiogenic heat production and on the real thermal conductivity (TC) of crystalline rocks of India. This
ETC, amounting to about 3.45 W/m·K, is 1.4 time greater than the mean real TC value (about 2.5 W/m·K). This is in good agreement
with the empirical relation between the surface heat flow density and the Curie depth for the Indian Craton. 相似文献
217.
218.
The paper summarises the history of human settlement in the Sudetes from the Bronze Age. A more intensive stage was reached
in the Middle Ages when settlers from the west established new villages deep in the mountain valleys. By the beginning of
the 20th century the Sudetes were already overpopulated but after a near-complete ethnic replacement from a German to a Polish
population in 1945–8, population continued to grow until the 1980s. However, the economic system was hardly sustainable by
this time. There were many polluting industries in the region and massive transboundary pollution from adjacent areas of Czechoslovakia
and Germany had a devastating effect on the forests. Moreover, subsidised state agriculture placed heavy pressure on vulnerable
mountain grazings. Since 1989 there has been a process of deindustrialisation in the Sudetes and surrounding areas and, with
the disappearance of the state farms and the reduction in subsidies, agriculture is now better adjusted to the natural potential
and is complemented by a promising start with agrotourism. The population of the region is growing relatively slowly (0.8%
per annum 1956–1999), with the rural areas now in decline. A sustainable future for the region is now a possibility, but while
there is a consensus for continued environmental reconstruction, supported by alternative economies, this will have to be
carefully managed in the years ahead when EU accession may bring heavier development pressures than those evident at the moment.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
219.
The vermiculite-like minerals show varied relative intensities of basal reflections and do not collapse fully when saturated with K and heated up to 700°C.
Transmission oblique texture X-ray diffraction patterns were used to determine a continuous series of the vermiculite-chlorite intermediate structures. Relative diffraction intensities in the region (060) were correlated with the amount of water released at 500–700°C to show that the investigated samples belong to two structurally distinctive series: vermiculitic and chloritic types. The structural premises indicate that the parent mineral for the chloritic intergrades should be chlorite and that for the vermiculitic series phlogopite. 相似文献
220.
Some ilmenite concentrates obtained from oleate flotation of ilmenite ores from NE Poland contain less than the required 45% TiO2 due to the presence of green spinels (hercynite and pleonaste). Such concentrates were further upgraded by different separation techniques. It was established at microlaboratory scale that magnetic, gravity and high-tension separations can provide qualified ilmenite concentrates with TiO2 recovery in the order of 50 to 80%. 相似文献