全文获取类型
收费全文 | 27123篇 |
免费 | 688篇 |
国内免费 | 1588篇 |
专业分类
测绘学 | 1518篇 |
大气科学 | 2522篇 |
地球物理 | 5244篇 |
地质学 | 13050篇 |
海洋学 | 1318篇 |
天文学 | 1818篇 |
综合类 | 2377篇 |
自然地理 | 1552篇 |
出版年
2024年 | 20篇 |
2023年 | 69篇 |
2022年 | 120篇 |
2021年 | 149篇 |
2020年 | 113篇 |
2019年 | 133篇 |
2018年 | 4864篇 |
2017年 | 4120篇 |
2016年 | 2695篇 |
2015年 | 386篇 |
2014年 | 241篇 |
2013年 | 183篇 |
2012年 | 1143篇 |
2011年 | 2880篇 |
2010年 | 2123篇 |
2009年 | 2454篇 |
2008年 | 2022篇 |
2007年 | 2459篇 |
2006年 | 175篇 |
2005年 | 306篇 |
2004年 | 486篇 |
2003年 | 484篇 |
2002年 | 307篇 |
2001年 | 132篇 |
2000年 | 158篇 |
1999年 | 172篇 |
1998年 | 143篇 |
1997年 | 142篇 |
1996年 | 115篇 |
1995年 | 80篇 |
1994年 | 104篇 |
1993年 | 81篇 |
1992年 | 56篇 |
1991年 | 35篇 |
1990年 | 51篇 |
1989年 | 27篇 |
1988年 | 30篇 |
1987年 | 18篇 |
1986年 | 15篇 |
1985年 | 11篇 |
1984年 | 8篇 |
1983年 | 7篇 |
1982年 | 13篇 |
1981年 | 27篇 |
1980年 | 23篇 |
1979年 | 5篇 |
1978年 | 1篇 |
1976年 | 7篇 |
1965年 | 1篇 |
1958年 | 5篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
41.
42.
43.
Using analytic signal method, interpretation of pole-pole secondary electric potentials due to 2D conductive/resistive prisms
is presented. The estimated parameters are the location, lateral extent or width and depth to top surface of the prism. Forward
modelling is attempted by 2D-Finite Difference method. The proposed stabilised analytic signal algorithm (RES2AS) uses Tikhonov’s
regularization scheme and FFT routines. The algorithm is tested on three theoretical examples and field data from the campus
of Roorkee University. The stability of RES2AS is also tested on synthetic error prone secondary pole-pole potential data. 相似文献
44.
45.
46.
47.
本文介绍了瑶沟等地区勘查金矿的放射性和非放射性气体地球化学方法的研究成果:基本查明了应用本方法勘查金矿的主要条件是金矿中伴生有足够的U,Hg和碳酸盐矿物;研制成了壤中气(Rn-CO2)联测技术,提高了测量质量和探测深部矿体的能力;利用壤中气(Rn-CO2)异常进行了成矿预测,并已获得成功。 相似文献
48.
Properties of wave velocity for two types of granitoids at high pressure and temperature and their geological meaning 总被引:1,自引:0,他引:1
Shufeng Yang Hanlin Chen Jishuang Jiang Guoqiang Zhu Hongshen Xie Wei Hou Yueming Zhang Huigang Xu 《中国科学D辑(英文版)》1997,40(5):470-476
The wave velocity for two types of granitoids was measured using the analytic method of full-wave vibration at high pressure
and high temperature. The laws of velocity changes for them differ with the pressure boost and temperature rise, and the velocity
change of S-type is more violent than that of I-type. The “softening point” of compressional wave velocity (V μ) is also revealed
during the measurement for two types of granitoids imitating the pressure and temperature at a certain depth. But the depth
of “softening”, Vp after “softening” and the percentage of Vp’s drop around the “sofrening point” for two types of granitoids are obviously different. The depth of “softening” is 15 km
approximately and Vp after “softening” is 5.62 km/s for S-type granitoid. But for I-type granitoid the depth of “softening” is 26 km approximately
and Vp after “softening” is 6. 08 km/s. Through careful analysis of rock slices after the experiment, it was found that the “softening”
of elastic-wave velocity is caused by the partial melting of granite. Combined with the results of geophysical prospecting,
these results suggest that the low-velocity layers developing in the interior of Earth crust are related to thc partial melting
of different types of granitoids. The formation of the low-velocity layer in the upper-middle Earth crust is closely related
to the development of S-type granitoid, but that in the lower Earth crust is closely related to the development of I-type
granitoid. 相似文献
49.
Zhengtong Xie Peter R. Voke Paul Hayden Alan G. Robins 《Boundary-Layer Meteorology》2004,111(3):417-440
A family of wall models is proposed that exhibits moresatisfactory performance than previousmodels for the large-eddy simulation (LES) of the turbulentboundary layer over a rough surface.The time and horizontally averaged statistics such asmean vertical profiles of windvelocity, Reynolds stress, turbulent intensities, turbulentkinetic energy and alsospectra are compared with wind-tunnel experimental data.The purpose of the present study is to obtain simulatedturbulent flows that are comparable with wind-tunnelmeasurements for use as the wind environment for thenumerical prediction by LES of source dispersion in theneutral atmospheric boundary layer. 相似文献
50.
Yijun Zhagn Wansheng Dong Yang Zhao Guangshu Zhang Hongfa Zhang Chengpin Chen Tong Zhang 《中国科学D辑(英文版)》2004,47(1):108-114
The comprehensive observations on lightning discharges were conducted in Naqu area of Qinghai-Tibet Plateau in summer of 2002. The electric structures of thunderstorms and the characteristics of lightning discharges at initial stage were analyzed by using the observation data. The results show that most of intracloud (IC) lightning flashes were polarities inverted in thunderstorms with tripole electric charge structure and occurred between negative charge region located in the middle of the thunderstorm and positive charge region located at the bottom of the thunderstorm. The radiation characteristics of discharge processes in cloud with longer lasting time involved in Cloud-to-Ground (CG) lightning flashes were similar to that of IC discharges. A lot of radiation pulses were produced in these discharge processes. Because the IC discharges took place at the bottom of thundercloud and were near the ground, they may produce more serious damage to equipment on the ground therefore should not be neglected in lightning protection. 相似文献