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   122篇
  免费   2篇
  国内免费   3篇
测绘学   7篇
大气科学   10篇
地球物理   21篇
地质学   44篇
天文学   38篇
综合类   3篇
自然地理   4篇
  2021年   3篇
  2020年   2篇
  2019年   2篇
  2018年   3篇
  2017年   4篇
  2016年   10篇
  2015年   4篇
  2014年   7篇
  2013年   7篇
  2012年   9篇
  2011年   11篇
  2010年   3篇
  2009年   6篇
  2008年   5篇
  2007年   3篇
  2006年   5篇
  2005年   2篇
  2004年   1篇
  2003年   2篇
  2002年   3篇
  1999年   2篇
  1998年   3篇
  1996年   2篇
  1994年   1篇
  1993年   2篇
  1992年   5篇
  1990年   3篇
  1989年   2篇
  1988年   1篇
  1987年   1篇
  1985年   2篇
  1982年   1篇
  1981年   3篇
  1978年   2篇
  1972年   1篇
  1971年   1篇
  1968年   1篇
  1967年   1篇
  1963年   1篇
排序方式: 共有127条查询结果,搜索用时 15 毫秒
121.
122.
A relationship between the melting temperature of a metal and its surface energy is used to predict, in a semi-empirical way, the variation of the melting temperature with pressure for sodium. The agreement of the predicted results with the experiments is very good.  相似文献   
123.
Summary Electron probe analysis of a bauxite sample with the highest content of the rare earth elements from the Nazda bauxite deposit in the Vlasenica bauxite-bearing area, revealed the presence of neodymian goyazite, a mineral of the crandallite group. Its composition lies between goyazite, florencite and crandallite, and can be described asCn 24Fc33Gz43. The first analyses of this mineral in bauxites are presented and the genesis is discussed.
Nd-haltiger Goyazit im Bauxitlager von Vlasenica, Jugoslawien
Zusammenfassung Ein Mineral der Crandallitgruppe, Neodym-Goyazit, wurde mittels Mikrosondenanalysen aus dem mit höchsten Gehalten an Seltenen Erden gekennzeichneten Nazda Bauxitlager im Vlasenica Bauxitgebiet identifiziert. Die Zusammensetzung liegt zwischen Goyazit, Florencit und Crandallit und kann mitCn 24Fc33Gz43 angegeben werden. Ein Überblick über die ersten Analysen dieses Minerals von Bauxitlagerstätten und seinen Ursprung wird hiermit gegeben.


With 3 Figures  相似文献   
124.
A broader consensus on the number of ground motions to be used and the method of scaling to be adopted for nonlinear response history analysis (RHA) of structures is yet to be reached. Therefore, in this study, the effects of selection and scaling of ground motions on the response of seismically isolated structures, which are routinely designed using nonlinear RHA, are investigated. For this purpose, isolation systems with a range of properties subjected to bidirectional excitation are considered. Benchmark response of the isolation systems is established using large sets of unscaled ground motions systematically categorized into pulse-like, non-pulse-like, and mixed set of motions. Different subsets of seven to 14 ground motions are selected from these large sets using (a) random selection and (b) selection based on the best match of the shape of the response spectrum of ground motions to the target spectrum. Consequences of weighted scaling (also commonly referred to as amplitude scaling or linear scaling) as well as spectral matching are investigated. The ground motion selection and scaling procedures are evaluated from the viewpoint of their accuracy, efficiency, and consistency in predicting the benchmark response. It is confirmed that seven time histories are sufficient for a reliable prediction of isolation system displacement demands, for all ground motion subsets, selection and scaling procedures, and isolation systems considered. If ground motions are selected based on their best match to the shape of the target response spectrum (which should be preferred over randomly selected motions), weighted scaling should be used if pulse-like motions are considered, either of weighted scaling or spectral matching can be used if non-pulse-like motions are considered, and an average of responses from weighted-scaled and spectrum-matched ground motions should be used for a mixed set of motions. On the other hand, the importance of randomly selected motions in representing inherent variability of response is recognized and it is found that weighted scaling is more appropriate for such motions.  相似文献   
125.
126.
127.
Finite‐difference P‐SV simulations of seismic scattering characteristics of faulted coal‐seam models have been undertaken for near‐surface P‐ and S‐wave sources in an attempt to understand the efficiency of body‐wave to channel‐wave mode conversion and how it depends on the elastic parameters of the structure. The synthetic seismograms clearly show the groups of channel waves generated at the fault: one by the downgoing P‐wave and the other by the downgoing S‐wave. These modes travel horizontally in the seam at velocities less than the S‐wavespeed of the rock. A strong Airy phase is generated for the fundamental mode. The velocity contrast between the coal and the host rock is a more important parameter than the density contrast in controlling the amplitude of the channel waves. The optimal coupling from body‐wave energy to channel‐wave energy occurs at a velocity contrast of 1.5. Strong guided waves are produced by the incident S‐sources for source angles of 75° to 90° (close to the near‐side face of the fault). As the fault throw increases, the amplitude of the channel wave also increases. The presence of a lower‐velocity clay layer within the coal‐seam sequence affects the waveguiding characteristics. The displacement amplitude distribution is shifted more towards the lower‐wavespeed layer. The presence of a ‘washout’ zone or a brecciated zone surrounding the fault also results in greater forward scattering and channel‐wave capture by the coal seam.  相似文献   
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