首页 | 本学科首页   官方微博 | 高级检索  
文章检索
  按 检索   检索词:      
出版年份:   被引次数:   他引次数: 提示:输入*表示无穷大
  收费全文   12082篇
  免费   2903篇
  国内免费   1594篇
测绘学   66篇
大气科学   28篇
地球物理   7554篇
地质学   6704篇
海洋学   591篇
天文学   10篇
综合类   683篇
自然地理   943篇
  2024年   59篇
  2023年   231篇
  2022年   372篇
  2021年   437篇
  2020年   502篇
  2019年   588篇
  2018年   440篇
  2017年   449篇
  2016年   501篇
  2015年   545篇
  2014年   730篇
  2013年   655篇
  2012年   712篇
  2011年   751篇
  2010年   667篇
  2009年   698篇
  2008年   662篇
  2007年   831篇
  2006年   829篇
  2005年   674篇
  2004年   698篇
  2003年   615篇
  2002年   535篇
  2001年   404篇
  2000年   434篇
  1999年   373篇
  1998年   349篇
  1997年   294篇
  1996年   326篇
  1995年   263篇
  1994年   242篇
  1993年   206篇
  1992年   142篇
  1991年   83篇
  1990年   57篇
  1989年   61篇
  1988年   50篇
  1987年   41篇
  1986年   31篇
  1985年   8篇
  1984年   3篇
  1982年   1篇
  1981年   4篇
  1980年   2篇
  1979年   16篇
  1954年   8篇
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
171.
In this study, observed seismic attributes from shot gather 11 of the SAREX experiment are used to derive a preliminary velocity and attenuation model for the northern end of the profile in southern Alberta. Shot gather 11 was selected because of its prominent Pn arrivals and good signal to noise ratio. The 2-D Gaussian beam method was used to perform the modeling of the seismic attributes including travel times, peak envelope amplitudes and pulse instantaneous frequencies for selected phases. The preliminary model was obtained from the seismic attributes from shot gather 11 starting from prior tomographic results. The amplitudes and instantaneous frequencies were used to constrain the velocity and attenuation structure, with the amplitudes being more sensitive to the velocity gradients and the instantaneous frequencies more sensitive to the attenuation structure. The resulting velocity model has a velocity discontinuity between the upper and lower crust, and lower velocity gradients in the upper and lower crust compared to earlier studies. The attenuation model has Q p -1 values between 0.011 and 0.004 in the upper crust, 0.0019 in the lower crust and a laterally variable Q p -1 in the upper mantle. The Q p -1 values are similar to those found in Archean terranes from other studies. Although the results from a single gather are non-unique, the initial model derived here provides a self-consistent starting point for a more complete seismic attribute inversion for the velocity and attenuation structure.  相似文献   
172.
Seismic structural control using semi-active tuned mass dampers   总被引:8,自引:1,他引:8  
This paper focuses on how to determine the instantaneous damping of the semi-active tuned mass damper (SATMD) with continuously variable damping. An off-and-towards-equilibrium (OTE) algorithm is employed to examine the control performance of the structure/SATMD system by considering the damping as an assumptive control action. The damping modification of the SATMD is carried out according to the proposed OTE algorithm, which is formulated based on analysis of the structural movement under external excitations, and the measured responses of the structure at every time instant. As examples two numerical simulations of a five-storey and a ten-storey shear structures with a SATMD on the roof are conducted. The effectiveness on vibration reduction of MDOF systems subjected to seismic excitations is discussed. Analysis results show that the behavior of the structure with a SATMD is significantly improved and the feasibility of applying the OTE algorithm to the structural control design of SATMD is also verified.  相似文献   
173.
On the basis of growing evidence thatstrong earthquakes are preceded by a periodof accelerating seismicity of moderatemagnitude earthquakes, an attempt is madeto search for such seismicity pattern in NWAegean area. Accelerating seismic crustaldeformation has been identified in the areaof southern Albanides mountain range(border region between Greece, formerYugoslavia and Albania). Based on certainproperties of this activity and on itssimilarity with accelerating seismicdeformation observed before a strongearthquake which occurred in the sameregion on 26 May 1960 (M = 6.5), we canconclude that a similar earthquake may begenerated in the same region during thenext few years. This conclusion is inagreement with independent results whichhave been derived on the basis of the timepredictable model.  相似文献   
174.
175.
176.
177.
178.
179.
180.
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号