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   39050篇
  免费   752篇
  国内免费   248篇
测绘学   766篇
大气科学   2615篇
地球物理   7722篇
地质学   14182篇
海洋学   3581篇
天文学   8757篇
综合类   88篇
自然地理   2339篇
  2022年   270篇
  2021年   446篇
  2020年   512篇
  2019年   586篇
  2018年   1018篇
  2017年   1029篇
  2016年   1101篇
  2015年   595篇
  2014年   1042篇
  2013年   1866篇
  2012年   1208篇
  2011年   1656篇
  2010年   1453篇
  2009年   1815篇
  2008年   1644篇
  2007年   1710篇
  2006年   1573篇
  2005年   1069篇
  2004年   1087篇
  2003年   1120篇
  2002年   1007篇
  2001年   875篇
  2000年   797篇
  1999年   726篇
  1998年   722篇
  1997年   726篇
  1996年   591篇
  1995年   573篇
  1994年   502篇
  1993年   454篇
  1992年   410篇
  1991年   425篇
  1990年   439篇
  1989年   394篇
  1988年   369篇
  1987年   400篇
  1986年   418篇
  1985年   508篇
  1984年   546篇
  1983年   542篇
  1982年   498篇
  1981年   454篇
  1980年   429篇
  1979年   408篇
  1978年   375篇
  1977年   384篇
  1976年   344篇
  1975年   353篇
  1974年   340篇
  1973年   370篇
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
191.
Abstract— The 50,000 year old, 1.8 km diameter Lonar crater is one of only two known terrestrial craters to be emplaced in basaltic target rock (the 65 million year old Deccan Traps). The composition of the Lonar basalts is similar to martian basaltic meteorites, which establishes Lonar as an excellent analogue for similarly sized craters on the surface of Mars. Samples from cores drilled into the Lonar crater floor show that there are basaltic impact breccias that have been altered by post‐impact hydrothermal processes to produce an assemblage of secondary alteration minerals. Microprobe data and X‐ray diffraction analyses show that the alteration mineral assemblage consists primarily of saponite, with minor celadonite, and carbonate. Thermodynamic modeling and terrestrial volcanic analogues were used to demonstrate that these clay minerals formed at temperatures between 130°C and 200°C. By comparing the Lonar alteration assemblage with alteration at other terrestrial craters, we conclude that the Lonar crater represents a lower size limit for impact‐induced hydrothermal activity. Based on these results, we suggest that similarly sized craters on Mars have the potential to form hydrothermal systems, as long as liquid water was present on or near the martian surface. Furthermore, the Fe‐rich alteration minerals produced by post‐impact hydrothermal processes could contribute to the minor iron enrichment associated with the formation of the martian soil.  相似文献   
192.
We are investigating the hypothesis that Compact High-Velocity Clouds (CHVCs) are the left-over building blocks of Local Group galaxies. To this end, we are searching for their embedded stellar populations using FORS at the VLT. The search is done with single-star photometry in V and I bands, which is sensitive to both, young and old, stellar populations. Five CHVCs of our sample have been observed so far down to I=24. We pointed the VLT towards the highest HI column density regions, as determined in Effelsberg radio data. In an alternate approach, we searched 2MASS public data towards those 5 CHVCs down to K=16. While the VLT data probe the central regions out to distance moduli of about 27, the 2MASS data are sensitive to a population of red giant stars to distance moduli of about 20. The 2MASS data, on the other hand, cover a much wider field of view than the VLT data (radius of 1 degree versus FORS field of 6.8 arcmin). We did not find a stellar population intrinsic to the CHVCs in either data. In this paper, we illustrate our search methods. This revised version was published online in August 2006 with corrections to the Cover Date.  相似文献   
193.
194.
195.
196.
197.
198.
199.
200.
 A steady radon exhalation is assumed in most publications. In a village of North-East Hungary, however, high radon concentrations have been measured, differing strongly in neighbouring houses and varying in time, due to the interplay of geochemical phenomena. Received: 20 November 1995 · Accepted: 18 June 1996  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