全文获取类型
收费全文 | 4893篇 |
免费 | 956篇 |
国内免费 | 1242篇 |
专业分类
测绘学 | 180篇 |
大气科学 | 1174篇 |
地球物理 | 1520篇 |
地质学 | 2232篇 |
海洋学 | 609篇 |
天文学 | 231篇 |
综合类 | 525篇 |
自然地理 | 620篇 |
出版年
2024年 | 19篇 |
2023年 | 86篇 |
2022年 | 207篇 |
2021年 | 271篇 |
2020年 | 176篇 |
2019年 | 257篇 |
2018年 | 286篇 |
2017年 | 244篇 |
2016年 | 294篇 |
2015年 | 238篇 |
2014年 | 329篇 |
2013年 | 263篇 |
2012年 | 291篇 |
2011年 | 295篇 |
2010年 | 298篇 |
2009年 | 270篇 |
2008年 | 272篇 |
2007年 | 246篇 |
2006年 | 222篇 |
2005年 | 186篇 |
2004年 | 143篇 |
2003年 | 178篇 |
2002年 | 151篇 |
2001年 | 129篇 |
2000年 | 162篇 |
1999年 | 191篇 |
1998年 | 193篇 |
1997年 | 171篇 |
1996年 | 153篇 |
1995年 | 169篇 |
1994年 | 134篇 |
1993年 | 135篇 |
1992年 | 95篇 |
1991年 | 56篇 |
1990年 | 51篇 |
1989年 | 51篇 |
1988年 | 44篇 |
1987年 | 42篇 |
1986年 | 26篇 |
1985年 | 14篇 |
1984年 | 11篇 |
1983年 | 8篇 |
1982年 | 9篇 |
1981年 | 6篇 |
1980年 | 6篇 |
1979年 | 1篇 |
1978年 | 3篇 |
1977年 | 4篇 |
1976年 | 1篇 |
1958年 | 4篇 |
排序方式: 共有7091条查询结果,搜索用时 0 毫秒
91.
This paper is a brief account of the essential points of geomechanics initited in China by Prof. J. S. Lee in the 1920's and some important results achieved by some Chinese petroleum geologists in recent years by applying geomechanics to the exploration and prospecting of oil and gas in eastern China. 相似文献
92.
关于热水沉积物稀土配分模式的讨论 总被引:5,自引:0,他引:5
海底热水沉积物的稀土配分模式取决于流体的密度和流方式,低密度热流体的沉积物稀配合模式类似于海水模式,高密度热流体的沉积物没有固定的稀土配分模式,在判别热水沉积物时不宜单独使用稀土配分模式。 相似文献
93.
Fen-Fei Wang Jian-Jun Liu Chun-Lai Li Xin Ren Ling-Li Mu Wei Yan Wen-Rui Wang Jing-Tao Xiao Xu Tan Xiao-Xia Zhang Xiao-Duan Zou Xing-Ye Gao 《中国天文和天体物理学报》2014,(12)
The establishment of a lunar control network is one of the core tasks in selenodesy, in which defining an absolute control point on the Moon is the most important step. However, up to now, the number of absolute control points has been very sparse. These absolute control points have mainly been lunar laser ranging retroreflectors, whose geographical location can be observed by observations on Earth and also identified in high resolution lunar satellite images. The Chang'e-3(CE-3) probe successfully landed on the Moon, and its geographical location has been monitored by an observing station on Earth. Since its positional accuracy is expected to reach the meter level, the CE-3 landing site can become a new high precision absolute control point. We use a sequence of images taken from the landing camera, as well as satellite images taken by CE-1 and CE-2, to identify the location of the CE-3 lander. With its geographical location known, the CE-3 landing site can be established as a new absolute control point, which will effectively expand the current area of the lunar absolute control network by 22%, and can greatly facilitate future research in the field of lunar surveying and mapping, as well as selenodesy. 相似文献
94.
Determining the location of buried plastic water pipes from measurements of ground surface vibration
J.M. MuggletonY. Gao 《Journal of Applied Geophysics》2011,75(1):54-61
‘Mapping the Underworld’ is a UK-based project, which aims to create a multi-sensor device that combines complementary technologies for remote buried utility service detection and location. One of the technologies to be incorporated in the device is low-frequency vibro-acoustics, and techniques for detecting buried infrastructure, in particular plastic water pipes, are being investigated. One of the proposed techniques involves excitation of the pipe at some known location with concurrent vibrational mapping of the ground surface in order to infer the location of the remainder of the pipe. In this paper, measurements made on a dedicated pipe rig are reported. Frequency response measurements relating vibrational velocity on the ground to the input excitation were acquired. Contour plots of the unwrapped phase revealed the location of the pipe to within 0.1-0.2 m. Magnitude contour plots revealed the excitation point and also the location of the pipe end. By examining the unwrapped phase gradients along a line above the pipe, it was possible to identify the wave-type within the pipe responsible for the ground surface vibration. Furthermore, changes in the ground surface phase speed computed using this method enabled the location of the end of the pipe to be confirmed. 相似文献
95.
96.
Sheng-Ping Gong Yun-Feng Gao Jun-Feng Li School of Aerospace Tsinghua University Beijing China 《中国天文和天体物理学报》2011,(8)
The fuel consumption associated with some interplanetary transfer trajectories using chemical propulsion is not affordable. A solar sail is a method of propulsion that does not consume fuel. Transfer time is one of the most pressing problems of solar sail transfer trajectory design. This paper investigates the time-optimal interplanetary transfer trajectories to a circular orbit of given inclination and radius. The optimal control law is derived from the principle of maximization. An indirect method is used... 相似文献
97.
渤海湾北岸晚新生代沉积环境和沉积体系不仅是区域水文地质、工程地质的基础,也为古近纪沉积模式提供“将今论古”的依据。本文依据沉积物色度和粒度,以及沉积物岩性、结构和构造等,将渤海湾北岸TZ02孔划分了6个沉积组合、4个沉积阶段:1)2.10~3.22Ma,沉积组合Ⅰ和Ⅱ,湖盆填充期,发育湖相-泛滥平原相或湖相-曲流河相,该时期处于构造稳定期,干冷气候时期发育河流相、泛滥平原相,湿润气候时期发育湖泊相。2)1.33~2.10Ma,沉积组合Ⅲ,湖盆开始发育期,主要为浅湖相,仅有少量砂体,下部多有机质,上部多钙质淀积结核,指示了盆山之间的构造分异后,湖泊初始发育的特征。3)0.62~1.33Ma,沉积组合Ⅳ,湖盆扩张期,以湖相为主,多砂体,且有短期湖泊水位变浅和成陆过程;指示了盆山构造分异后,盆地加速沉降,湖盆扩张;山体隆起、河流下切,盆地中湖相砂体增多;此时TZ02孔附近为湖相中心,BG10孔为湖泊边缘。4)0~0.62Ma,沉积组合Ⅴ和Ⅵ,湖泊填充期,BG10孔为湖相的沉积中心,而TZ02孔为湖泊的边缘,接受滦河迁移摆动后的沉积物;中更新世后,构造沉降形成湖相,而间冰期发育海相,埋深0~22.5m的海相-河流相更直接地反映了末次冰消期海平面变化过程。
相似文献98.
Han Wenliang Gao Guoming Wang Guangqian Hui Yujia Department of Hydraulic Engineering Tsinghua University Beijing China 《国际泥沙研究》2000,(3)
I INTRODUCTIONThe settlement of particles in fluid has been studied in many fields such as hydraulics, metallurgy andchemistry since the middle of 19 century because of its great importance. Although the settlement ofsingle particle and group settling velocity of uniform particles in still water are relatively well-studied, yetthe settlement of non-uniform particles in flowing water lacks understanding. For instance, Cunningham(1910), Richardson (1954) and Batchelor (1972), have obtained… 相似文献
99.
Avalanche in Tuban: a hazard with no defense 总被引:1,自引:0,他引:1
Xiang-Zhou Xu Guo-Dong Song Jie Liu Wei-Qin Dang Hang Gao Zhen-Yi Liu Hong-Wu Zhang 《Natural Hazards》2015,79(3):2181-2187
100.
中国西北部“4.5”沙尘暴过程中尺度低压的数值模拟 总被引:3,自引:9,他引:3
利用改进型PSU/NCAR中尺度数值模式(MM4标准版),取模式水平格距40km,46×61网格,垂直方向a取15层,即从地面到模式顶(100hPa),σ=0.0、0.1、0.2、0.3、0.4、0.5、0.6、0.7、0.78、0.84、0.89、0.93、0.96、0.98、0.99、1.00,采用NCAR的30'×30'地形资料,以常规观测资料作为初始场,较好地模拟了此次沙尘暴过程的海平面气压的演变和分布,特别是张掖、柴达本盆地以及敦煌附近的三个中低压。同时,模拟了张掖中低压与蒙古冷高压之间的甘肃河西沙尘暴东大风。敏感性试验表明,沙尘暴中低压的形成发展主要是受于物理过程制约;沙尘暴中尺度系统的研究与暴雨中尺度系统的研究是有区别的,积云对流参数化并不是特别重要,在设计研究沙尘暴的数值模式中,应当合理地处理其他的热力、动力过程及大气外强迫源的作用。模式水平格距、地形真实程度对模拟中低压的位置、中心强度有重要贡献;下垫面变化中低压强度有一定影响。张掖热低压的形成发展主要是在有利的环境形势下,特殊地势起了重要作用,表现为直接动力强迫和间接热力强迫。 相似文献