全文获取类型
收费全文 | 5200篇 |
免费 | 1150篇 |
国内免费 | 1518篇 |
专业分类
测绘学 | 785篇 |
大气科学 | 838篇 |
地球物理 | 1345篇 |
地质学 | 2832篇 |
海洋学 | 835篇 |
天文学 | 110篇 |
综合类 | 431篇 |
自然地理 | 692篇 |
出版年
2024年 | 83篇 |
2023年 | 202篇 |
2022年 | 412篇 |
2021年 | 468篇 |
2020年 | 350篇 |
2019年 | 411篇 |
2018年 | 405篇 |
2017年 | 382篇 |
2016年 | 382篇 |
2015年 | 363篇 |
2014年 | 396篇 |
2013年 | 368篇 |
2012年 | 393篇 |
2011年 | 405篇 |
2010年 | 369篇 |
2009年 | 343篇 |
2008年 | 344篇 |
2007年 | 281篇 |
2006年 | 215篇 |
2005年 | 176篇 |
2004年 | 157篇 |
2003年 | 133篇 |
2002年 | 182篇 |
2001年 | 163篇 |
2000年 | 100篇 |
1999年 | 72篇 |
1998年 | 37篇 |
1997年 | 46篇 |
1996年 | 35篇 |
1995年 | 25篇 |
1994年 | 25篇 |
1993年 | 23篇 |
1992年 | 20篇 |
1991年 | 12篇 |
1990年 | 21篇 |
1989年 | 14篇 |
1988年 | 18篇 |
1987年 | 3篇 |
1986年 | 10篇 |
1985年 | 4篇 |
1984年 | 2篇 |
1983年 | 5篇 |
1981年 | 2篇 |
1980年 | 2篇 |
1979年 | 2篇 |
1975年 | 1篇 |
1958年 | 1篇 |
1957年 | 2篇 |
1954年 | 3篇 |
排序方式: 共有7868条查询结果,搜索用时 0 毫秒
391.
为了深入研究密云射电源表分类样本的性质,作为系列工作的第一部分,选出了一个232~4850MHz平谱源样本.1998年5月29至31日,利用北京天文台2.16米望远镜和OMR摄谱仪,对其中18个目标进行了观测及光谱认证.结果共证认出15个AGN,其中3个信噪比不小于8的BLLac天体和5个类星体(最大红移为2.519±0.003)是新发现的. 相似文献
392.
本文介绍了云南天文台四波段(1.42,2.13,2.84和4.26GHz)太阳射电高时间分辩率同步观测得到的五个微波II型爆发事件,它们具有宽频带、长和短寿命、内向和外向快速频漂等特征.观测事例表明,非热电子束引起的等离子体辐射和电子回旋脉泽辐射两种机制都可能发生.这些观测特征既不完全同于米波—分米波II型爆发,也不完全同于微波高频段II型爆发,说明在微波低频段可能存在二重性或过渡现象 相似文献
393.
柴达木盆地东缘晚更新世气候变化的(古)土壤发生记录 总被引:4,自引:1,他引:3
柴达木盆地东缘典型剖面(古)土壤及其黄土线质的宏观特征和理化分析表明,本区晚更新世以来气候曾有几次较大的波动,反映了全球冰量影响的气候波动以及东亚季风气候的强弱变化特征。揭示出气候变化过程中温度和降水并不同步,温度主要受地球轨道变化引起的太阳辐射的影响;降水则主要取决于冬、夏季风的浊弱对比关系,夏季风盛行时,降水丰沛。间冰段古土壤Sm的土壤发生特征和强度,揭示了除低温引起的蒸发减少外,降水丰沛也是 相似文献
394.
颅脑外伤分类的CT特征 总被引:2,自引:2,他引:0
本文目的在于进一步提高对多种颅脑损伤的认识水平。所用材料和方法为本组135例,男98例,女37例,年龄4_77岁,平均年龄24.83岁。车祸伤93例,跌伤28例,击伤14伤,101例有昏迷史,全部病例均作头颅CT轴位平扫。从相互伴发的多种颅脑损伤的角度,详细分析了它们的CT表现。结果得到了135例中,有多种类型颅脑损伤133例,单纯脑挫裂伤2例;硬膜外血肿104例,合并同一部位骨折75例,占72.15%,合并脑挫裂伤占70.37%;硬膜下血肿20例,位于外力对冲部位15例.占75%,合并脑挫伤裂伤12例,其中11例邻近硬膜下血肿;外伤后2小时内CT检查,并于外伤后4小时至5天内CT复查47例,发现病变进展38例,占80.95%。结论为硬膜外血肿多伴同部位骨折;在硬膜外血肿中,伴发的脑挫裂伤多位于对冲部位;硬膜下血肿多发生于对冲部位;颅脑损伤后,短期内病变可能会继续发展。 相似文献
395.
The high-temperature and pressure experimental data of garnet, sillimantite and biotite-bearing potash feldspar gneiss (SGBG,
natural block rock) has shown that metamorphic reactions between garnet and melt, and mineral assemblage evolutional features
are not only controlled byP-T condition, but also genetically correlate with dehydration-melting of biotite and partial melting of felsic minerals. Combining
experimental data with theoretical analyses, the genetic mechanism of metamorphic reaction and its dynamic significance have
been demonstrated in the process of metamorphic evolution of khondalite series on the border of Jin (Shanxi Province)-Inner
Mongolia.
Project supported by the Youth Geologist Foundation of Ministry of Geology and Mineral Resources of China, the Post-docter
Foundation and the National Natural Science Foundation of China (Grant No. 49572138). 相似文献
396.
SHI Dehong YIN Xi SUN Jichao YIN ZhengzhouInstitute of Hydrogeology Engineering Geology CAGS Zhengding Hebei Province Zhou Jian Zhu Xiling 《《地质学报》英文版》1998,72(1):100-107
Three Cenozoic basins-the Qaidam basin, the Weihe graben-type basin and the North China plain-which are different in climatic conditions, geological settings and run-off types, are selected for the study. Based on an analysis of background information of the transect along the middle-latitude region, studies of groundwater dynamics, geochemistry, simulation of water circulation of the main elements as well as isotopic chronology, the information on global changes is collected, the formation of groundwater circulation systems and their evolution under stacked impacts of natural conditions and human activities are discussed, and a correlation is made between the evolutionary features of the above systems in these basins since 25 ka B.P. All these have laid a good foundation for further generalizing the evolutionary model of land water in northern China. 相似文献
397.
Dynamics of the three-dimensional structure of the wind-driven Deacon cell in a β-plane channel are discussed in a homogeneous model in the presence of a sufficiently high ridge. The emphasis is on the water mass balance: how the northward surface Ekman drift is returned. It is demonstrated that a sufficiently high ridge can break up the geostrophic constraint and a net geostrophic volume flux across the open latitude band is allowed. It is found that: (1) the Deacon cell is a fundamentally three-dimensional structure, (2) wind forcing can drive an inter-basin water mass exchange in the Southern Ocean, and (3) zonal through-channel transport in the circumpolar ocean varies at different longitudes. 相似文献
398.
José M. Marques Paula M. M. Carreira Luís Aires-Barros Rui C. Graça 《Environmental Geology》2000,40(1-2):53-63
At the northern part of the Portuguese mainland, the upflow zone of several hot and cold HCO3/Na/CO2-rich mineral waters is mainly associated with important NNE–SSW faults. Several geochemical studies have been carried out
on thermal and non-thermal hydromineral manifestations that occur along or near these long tectonic alignments. The slight
chemical differences that exist between these meteoric hot and cold HCO3/Na/CO2-rich mineral waters seem to be mainly caused by CO2. δ13C(TIDC) values observed in these groundwaters range between –6.00 and –1.00‰ versus V-PDB (V denotes Vienna, the site of the International
Atomic Energy Agency; PDB originates from the CaCO3 of the rostrum of a Cretaceous belemnite, Belemnitella americana, collected in the Peedee formation of South Carolina, USA) indicating a deep-seated (mantle) origin for most of the CO2. Nevertheless, in the case of the heavier δ13C(TIDC) values, the contribution of metamorphic CO2 or the dissolution of carbonate rock levels at depth cannot be excluded. Concerning the hot waters, the lack of a positive
18O-shift should be attributed to water-rock interaction in a low temperature environment, rather than to the isotopic influence
of CO2 on the δ18O-value of the waters.
Received: 9 August 1999 · Accepted: 8 March 2000 相似文献
399.
The soil freeze–thaw controls the hydrological and carbon cycling and thus affects water and energy exchanges at land surface. This article reported a newly developed algorithm for distinguishing the freeze/thaw status of surface soil. The algorithm was based on information from Advanced Microwave Scanning Radiometer Enhanced (AMSR‐E) which records brightness temperature (Tb) in the afternoon and after midnight. The criteria and discriminant functions were obtained from both radiometer observations and model simulations. First of all, the microwave radiation from freeze–thaw soil was examined by carrying out experimental measurements at 18·7 and 36·5 GHz using a Truck‐mounted Multi‐frequency Microwave Radiometer (TMMR) in the Heihe River of China. The experimental results showed that the soil moisture is a key component that differentiates the microwave radiation behaviours during the freeze–thaw process, and the differences in soil temperature and emissivity between frozen and thawed soils were found to be the most important criteria. Secondly, a combined model was developed to consider the impacts of complex ground surface conditions on the discrimination. The model simulations quite followed the trend of in situ observations with an overall relation coefficient (R) of approximately 0·88. Finally, the ratio of Tb18·7H (horizontally polarized Tb at 18·7 GHz) to Tb36·5V was considered primarily as the quasi‐emissivity, which is more reasonable and explicit in measuring the microwave radiation changes in soil freezing and thawing than the spectral gradient. By combining Tb36·5V to indicate the soil temperature variety, a Fisher linear discrimination analysis was used to establish the discriminant functions. After being corrected by TMMR measurements, the new discriminant algorithm had an overall accuracy of 86% when validated by 4‐cm soil temperature. The multi‐year discriminant results also provided a good agreement with the classification map of frozen ground in China. Copyright © 2011 John Wiley & Sons, Ltd. 相似文献
400.
Sérgio P. Ávila Patrícia Madeira C. Marques da Silva Mário Cachão Bernard Landau Rui Quartau A. M. de Frias Martins 《第四纪科学杂志》2008,23(8):777-785
The Pleistocene (Eemian) outcrops of Lagoinhas and Prainha, located at Santa Maria Island (Azores), were investigated and their fossil mollusc content reported. These studies revealed that the last glaciation affected two groups of molluscs: the ‘warm‐guest’ gastropods with West African or Caribbean affinities (e.g. Conus spp., Cantharus variegatus, Bulla amygdala, Trachypollia nodulosa) and shallow bivalve species mainly associated with sandy habitats (Ensis minor, Lucinella divaricata, and probably Laevicardium crassum). In this paper we focus on this group of bivalves, which has since locally disappeared from the Azores. We relate the local disappearance of these bivalves in the Azores with the lack of sand in the shelf. The specific characteristics of the Santa Maria shelf combined with the sea‐level drop during the Weichselian prevented deposition of the lowstand deposits and permitted erosion of the previous ones, leaving the shelf without a sediment cover. Copyright © 2008 John Wiley & Sons, Ltd. 相似文献