全文获取类型
收费全文 | 6815篇 |
免费 | 207篇 |
国内免费 | 81篇 |
专业分类
测绘学 | 231篇 |
大气科学 | 629篇 |
地球物理 | 1525篇 |
地质学 | 2523篇 |
海洋学 | 585篇 |
天文学 | 1161篇 |
综合类 | 24篇 |
自然地理 | 425篇 |
出版年
2022年 | 51篇 |
2021年 | 94篇 |
2020年 | 118篇 |
2019年 | 91篇 |
2018年 | 202篇 |
2017年 | 184篇 |
2016年 | 244篇 |
2015年 | 160篇 |
2014年 | 221篇 |
2013年 | 334篇 |
2012年 | 266篇 |
2011年 | 405篇 |
2010年 | 299篇 |
2009年 | 387篇 |
2008年 | 339篇 |
2007年 | 271篇 |
2006年 | 279篇 |
2005年 | 280篇 |
2004年 | 350篇 |
2003年 | 274篇 |
2002年 | 205篇 |
2001年 | 148篇 |
2000年 | 158篇 |
1999年 | 138篇 |
1998年 | 133篇 |
1997年 | 107篇 |
1996年 | 75篇 |
1995年 | 77篇 |
1994年 | 73篇 |
1993年 | 65篇 |
1992年 | 61篇 |
1991年 | 47篇 |
1990年 | 58篇 |
1989年 | 30篇 |
1988年 | 30篇 |
1987年 | 55篇 |
1986年 | 37篇 |
1985年 | 41篇 |
1984年 | 58篇 |
1983年 | 45篇 |
1982年 | 49篇 |
1981年 | 43篇 |
1980年 | 41篇 |
1979年 | 28篇 |
1978年 | 44篇 |
1977年 | 41篇 |
1976年 | 38篇 |
1975年 | 44篇 |
1974年 | 36篇 |
1973年 | 35篇 |
排序方式: 共有7103条查询结果,搜索用时 46 毫秒
191.
192.
Sabine Gaudzinski Felix Bittmann Wolfgang Boenigk Manfred Frechen Thijs Van Kolfschoten 《Quaternary Research》1996,46(3):319-334
The Kärlich–Seeufer archaeological site in Germany's central Rhineland was excavated between 1980 and 1992. The site provides evidence for hominid activity during a Middle Pleistocene interglaciation known up to now only from the Kärlich clay pit and therefore defined as the Kärlich Interglaciation, which is considered to be post-Cromer IV and pre-Holstein (sensu stricto) in age. The site is characterized by Acheulean artifacts, a fauna dominated byElephas (Palaeoloxodon) antiquus,and a unique and outstanding preservation of wooden and other palaeobotanical remains. Assuming all finds are associated, the site previously was interpreted as an elephant hunting camp with a wooden structure, together with wood and bone implements preservedin situ.Recent analysis of the same features has shown that the site can also be interpreted as a reworked archaeological sample. Hominid occupation occurred in the vicinity of a small lake with prevailing meso-oligotrophic conditions. Expanding boreal forests and fen vegetation characterized the landscape. 相似文献
193.
194.
During the last decade, exploration and mining of modern-Tertiary heavy mineral beach and raised beach sands along the west
coast of South Africa has developed into a major industry. High resolution radiometric techniques have demonstrated their
use as a quantitative indicator of total heavy mineral concentration (THM) and also have the ability to discriminate between
sediments derived from different provenance terrains. Results indicate that it is possible to calculate the total heavy mineral
concentration from high resolution radiometric measurements, but the ability to quantify the concentration of individual mineral
fractions, such as ilmenite, requires further refinement of the method. Radiometric characteristics of the light mineral fraction
made it possible to distinguish between sediments from mixed marine-aeolian palaeoplacers and active present beach placers.
The effects of in situ alteration of the ilmenite fraction in the palaeoplacers were also reflected by subtle contrasts in
the radiometric character of the deposits. Furthermore, the uniform radiometric character of the sample population indicates
a common provenance for the heavy mineral suite and supports previous results which indicate the metamorphites of the mid-Proterozoic
Namaqua Province as the primary source terrain. The high resolution radiometric techniques discussed offer a broad spectrum
of applications in sedimentology and have the potential to aid heavy mineral exploration. With further refinement it can possibly
be used quantitatively in grade control during mining and beneficiation of heavy mineral deposits.
Received: 19 July 1996 / Accepted: 7 January 1997 相似文献
195.
Geologie en Mijnbouw - 相似文献
196.
Geochemical exploration for platinum-group elements in the Bushveld Complex, South Africa 总被引:2,自引:0,他引:2
H. J. Wilhelm H. Zhang F. L. Chen J. H. Elsenbroek M. Lombard D. de Bruin 《Mineralium Deposita》1997,32(4):349-361
Analyses of stream sediment and soil samples from the Bushveld Complex, South Africa have revealed enhanced precious metal
concentrations, which can be related both to mining activities and the presence of hidden concentrations of platinum-group
elements (PGEs) and gold. The economically important PGE deposits hosted by the Upper Critical Zone of the Rustenburg Layered
Suite are revealed by a high PGE and Au content in the overlying soils. A second zone of elevated precious metal concentrations
straddles the boundary between the Main and Upper Zones and has to date been traced for more than 100 km. This zone follows
the igneous layering of the Rustenburg Layered Suite and is offset by the Brits Graben. It is therefore thought to be the
reflection of a magmatic PGE-Au mineralisation.
Received: 31 May 1996 / Accepted: 7 January 1997 相似文献
197.
198.
S. Klimov S. Romanov E. Amata J. Blecki J. Büchner J. Juchniewicz J. Rustenbach P. Triska L. J. C. Woolliscroft S. Savin Yu. Afanas’yev U. de Angelis U. Auster G. Bellucci A. Best F. Farnik V. Formisano P. Gough R. Grard V. Grushin G. Haerendel V. Ivchenko V. Korepanov H. Lehmann B. Nikutowski M. Nozdrachev S. Orsini M. Parrot A. Petrukovich J. L. Rauch K. Sauer A. Skalsky J. Slominski J. G. Trotignon J. Vojta R. Wronowski 《Annales Geophysicae》1997,15(5):514-527
The plasma-wave experiment ASPI (analysis of spectra of plasma waves and instabilities) on board the INTERBALL spacecraft is a combined wave diagnostics experiment. It performs measurements of the DC and AC magnetic field vector by flux-gate and searchcoil sensors, the DC and AC electric field vector by Langmuir double probes and the plasma current by Langmuir split probe. Preliminary data analysis shows the low noise levels of the sensors and the compatibility of new data with the results of previous missions. During several months of in-orbit operation a rich collection of data was acquired, examples of which at the magnetopause and plasma sheet are presented in second part of the paper. 相似文献
199.
Fluid inclusion leachates obtained from vug and vein quartz samples from an Archean (3.23 Ga) Fe-oxide hydrothermal deposit in the west-central part of the Barberton greenstone belt, South Africa, were analyzed by ion chromatography for chloride, bromide, and iodide. The deposit, known as the ironstone pods, formed by seafloor hydrothermal activity and fluid discharge. Quartz is dominated by type I liquid-vapor, aqueous inclusions with a bimodal salinity distribution (0–0.25 MCl− and 0.9–1.8 MCl−). Bulk analytical salinities range from 0.45 to 0.99 MCl− represent averages of type I inclusions. Bulk fluid inclusion bromide and iodide concentrations are 1.44–3.32 mM and 0.01–0.12 mM, respectively. For comparison, modern seawater has halogen contents of 590 mM chloride, 0.9 mM bromide, and 0.5 μM total iodine. In the fluids from the ironstone pods, bromide and iodide are enriched relative to chloride, when compared with modern seawater.Approximate Br−Cl− and I−Cl− ratios of 3.2 Ga Barberton seawater are 2.5 × 10−3 and 40 × 10−6, respectively. Dispersion to higher values was caused principally by reaction with organic sediments whose trends are similar to those seen for modern vent fluids at unsedimented and sedimented ridges, relative to modern seawater. These halide ratios are greater than those of modern seawater, suggesting a change in the halide ratios of seawater over geological time. The analytical data are consistent with a model in which marine organic sedimentation has fractionated bromine and iodine out of seawater relative to chloride, thereby causing the halide ratios of seawater to decrease from high early and mid-Archean values towards their present day values. 相似文献
200.
A regional atmospheric climate model is used toexamine the effect of changes in the roughnesslengths of momentum (z0m) and heat (z0h)on the structure of the lower atmosphere and on thesurface energy fluxes over Antarctica. Fourexperiments were carried out in which z0mand/or z0h were altered with respect to acontrol experiment. The changes consisted of (1) alowering of z0m from a field aggregated froma vegetation map with an orographic correction basedon the European Centre for Medium-Range WeatherForecasts z0m field, to a constant value of10-3 m; and (2) a lowering of z0h from a valueequal to z0m to a constant value of 10-3 mor a value dependent on the wind speed via a surfacerenewal model. A reduction of z0m results in theexpected increase in near-surface wind speed. It alsoresults in an increase in the depth of the layer in whichsouth-easterly near-surface winds prevail, and in adecrease in the strength of the large-scale flow overthe continent, in particular in summer. In theescarpment region a decrease of z0m is foundto result in too high wind speeds. Surface temperatureson average decrease while atmospheric temperaturesincrease, resulting in an increase of near-surfacestatic stability. Changes in roughness lengths donot significantly change the temperature profiles.The surface fluxes, on average found reduced, aremodelled best by using the z0h based on thesurface renewal method. 相似文献