全文获取类型
收费全文 | 12867篇 |
免费 | 3158篇 |
国内免费 | 4806篇 |
专业分类
测绘学 | 2469篇 |
大气科学 | 1944篇 |
地球物理 | 2268篇 |
地质学 | 7974篇 |
海洋学 | 3120篇 |
天文学 | 172篇 |
综合类 | 1172篇 |
自然地理 | 1712篇 |
出版年
2024年 | 122篇 |
2023年 | 326篇 |
2022年 | 881篇 |
2021年 | 1028篇 |
2020年 | 907篇 |
2019年 | 1087篇 |
2018年 | 917篇 |
2017年 | 922篇 |
2016年 | 908篇 |
2015年 | 945篇 |
2014年 | 959篇 |
2013年 | 1132篇 |
2012年 | 1197篇 |
2011年 | 1182篇 |
2010年 | 1050篇 |
2009年 | 1090篇 |
2008年 | 1058篇 |
2007年 | 983篇 |
2006年 | 906篇 |
2005年 | 677篇 |
2004年 | 506篇 |
2003年 | 400篇 |
2002年 | 381篇 |
2001年 | 370篇 |
2000年 | 269篇 |
1999年 | 115篇 |
1998年 | 67篇 |
1997年 | 57篇 |
1996年 | 59篇 |
1995年 | 38篇 |
1994年 | 40篇 |
1993年 | 25篇 |
1992年 | 23篇 |
1991年 | 20篇 |
1990年 | 15篇 |
1989年 | 7篇 |
1988年 | 14篇 |
1987年 | 16篇 |
1986年 | 22篇 |
1985年 | 11篇 |
1984年 | 18篇 |
1982年 | 11篇 |
1981年 | 7篇 |
1980年 | 11篇 |
1979年 | 4篇 |
1977年 | 4篇 |
1976年 | 4篇 |
1974年 | 6篇 |
1973年 | 4篇 |
1954年 | 11篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
111.
胶东半岛大磨曲家金矿床成矿流体物理化学条件演化 总被引:2,自引:1,他引:1
胶东大磨曲家金矿床流体包裹体包括水溶液包裹体、富CO2包裹体和高盐卤水包裹体3种类型,前两者发育较多,高盐卤水包裹体发育极少。流体包裹体显微测温及盐度、密度、压力估算显示,水溶液包裹体均一温度为98~376℃,据冰点温度估算,盐度为0.53%~8.28%,水溶液包裹体均一压力低于50×105Pa;富CO2包裹体完全均一温度为255~348℃,盐度为2.42%~11.43%,均一压力为1 000×105~2 500×105Pa;富CO2包裹体中CO2均一温度为23.0~32.4℃,指示该类包裹体可能含有数量不等的CH4或H2S。静水压力体制下,根据纯CO2包裹体均一压力估算成矿深度约为1 km。在270℃左右,均一压力从富CO2包裹体到水溶液包裹体急剧降低,指示成矿流体在270℃左右可能发生过一次减压沸腾过程,成矿流体盐度和密度在270℃左右也有显著的变化。因此,沸腾作用及其引起的成矿流体物理化学条件的急剧变化可能是导致大磨曲家金矿床成矿物质沉淀的重要机制。 相似文献
112.
113.
114.
115.
Environmental Investigation and Evaluation of Land Subsidence in the Datong Coalfield Based on InSAR Technology 总被引:1,自引:0,他引:1
Heavy mining of Jurassic and Carboniferous horizontal coal seams in the Datong coalfield has seriously affected the local geological environment, which is mainly manifested by such geohazards as soil avalanches, landslides, mudflows, surface subsidence, surface cracks, surface solid waste accumulation and surface deformation. More seriously, coal mining causes groundwater to leak. Overpumping of groundwater has resulted in substantial land subsidence of the urban area in Datong City. Based on the previous geo-environmental investigation in the work area, the authors used radar remote sensing techniques such as InSAR (synthetic aperture radar interferometry) and D-InSAR (differential synthetic aperture radar interferometry), supplemented by the optical remote sensing method, for geo-environmental investigation to ascertain the geo-environmental background of the Datong Jurassic and Carboniferous-Permian coalfield and evaluate the effects of the geohazards, thus providing a basis for the geo-environmental protection, geohazard control and prevention, land improvement and optimization of the human environment. In this study 8 cog-nominal ERS-1/2 SAR data frames during 1992 to 2003 were used, but the following processing was made: (1) the multitemporal SAR magnitude images were used to interpret the geological structure, vegetation, microgeomorphology and drainage system; (2) the multi-temporal InSAR coherent images were used to make a classification of surface features and evaluate the coherence change due to coal mining; and (3) the multi-temporal cog-nominal SAR images were used to complete D-InSAR processing to remove the information of differential deformation areas (sites). In the end, a ten-year time series of differential interferograms were obtained using the multi-temporal cog-nominal SAR images. In the tests, 84 deformed areas (sites) were obtained, belonging to those in 1993-1996, 1996-1997, 1997-1998, 1998-2001, 1998-2002 and 2001-2003 respectively. Of the 84 areas, 44 are m 相似文献
116.
Late Cenozoic Stratigraphy and Paleomagnetic Chronology of the Zanda Basin, Tibet, and Records of the Uplift of the Qinghai-Tibet Plateau 总被引:1,自引:0,他引:1
MENG Xiangang ZHU Dagang SHAO Zhaogang YANG Chaobin HAN Jianen YU Ji MENG Qingwei LU Rongping 《《地质学报》英文版》2008,82(1):63-72
The characteristics of Late Cenozoic tectonic uplift of the southern margin of the Qinghai- Tibet Plateau may be inferred from fluvio-lacustrine strata in the Zanda basin, Ngari, Tibet. Magnetostratigraphic study shows that the very thick fluvio-lacustrine strata in the basin are 5.89- 0.78 Ma old and that their deposition persisted for 5.11 Ma, i.e. starting at the end of the Miocene and ending at the end of the early Pleistocene, with the Quaternary glacial stage starting in the area no later than 1.58 Ma. Analysis of the sedimentary environment indicates that the Zanda basin on the southern Qinghai-Tibet Plateau began uplift at -5.89 Ma, later than the northern Qinghai-Tibet Plateau. Presence of gravel beds in the Guge and Qangze Formations reflects that strong uplift took place at -5.15 and -2.71 Ma, with the uplift peaking at -2.71 Ma. 相似文献
117.
118.
119.
120.
Wenbin Shen Jin Li Jiancheng Li Zhengtao Wang Jinsheng Ning Dingbo Chao 《地球空间信息科学学报》2008,11(4):273-278
Given the second radial derivative Vrr(P) |δs of the Earth's gravitational potential V(P) on the surface δS corresponding to the satellite altitude, by using the fictitious compress recovery method, a fictitious regular harmonic field rrVrr(P)^* and a fictitious second radial gradient field V:(P) in the domain outside an inner sphere Ki can be determined, which coincides with the real field V(P) in the domain outside the Earth. Vrr^*(P)could be further expressed as a uniformly convergent expansion series in the domain outside the inner sphere, because rrV(P)^* could be expressed as a uniformly convergent spherical harmonic expansion series due to its regularity and harmony in that domain. In another aspect, the fictitious field V^*(P) defined in the domain outside the inner sphere, which coincides with the real field V(P) in the domain outside the Earth, could be also expressed as a spherical harmonic expansion series. Then, the harmonic coefficients contained in the series expressing V^*(P) can be determined, and consequently the real field V(P) is recovered. Preliminary simulation calculations show that the second radial gradient field Vrr(P) could be recovered based only on the second radial derivative V(P)|δs given on the satellite boundary. Concerning the final recovery of the potential field V(P) based only on the boundary value Vrr (P)|δs, the simulation tests are still in process. 相似文献