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   263761篇
  免费   4699篇
  国内免费   4091篇
测绘学   7273篇
大气科学   19648篇
地球物理   55501篇
地质学   92018篇
海洋学   21918篇
天文学   56708篇
综合类   1194篇
自然地理   18291篇
  2021年   2399篇
  2020年   2708篇
  2019年   2949篇
  2018年   3760篇
  2017年   3424篇
  2016年   5907篇
  2015年   4360篇
  2014年   7076篇
  2013年   14406篇
  2012年   6851篇
  2011年   8382篇
  2010年   7296篇
  2009年   9987篇
  2008年   8826篇
  2007年   8274篇
  2006年   9934篇
  2005年   7933篇
  2004年   7782篇
  2003年   7276篇
  2002年   6882篇
  2001年   6129篇
  2000年   6029篇
  1999年   5239篇
  1998年   5272篇
  1997年   5075篇
  1996年   4705篇
  1995年   4456篇
  1994年   4135篇
  1993年   3887篇
  1992年   3676篇
  1991年   3615篇
  1990年   3787篇
  1989年   3538篇
  1988年   3318篇
  1987年   3872篇
  1986年   3426篇
  1985年   4250篇
  1984年   4765篇
  1983年   4437篇
  1982年   4339篇
  1981年   3954篇
  1980年   3655篇
  1979年   3520篇
  1978年   3490篇
  1977年   3287篇
  1976年   3050篇
  1975年   2965篇
  1974年   2928篇
  1973年   3086篇
  1972年   2034篇
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
991.
992.
993.
Seasonal changes in coccolithophore cell densities in the San Pedro Basin, Southern California Bight, were investigated for the period October 1991 to September 1992. Coccolitho phore cell densities ranged from 6.3 × 104 coccospheres per liter in March 1992 to 0 cells per liter in November 1991. High coccolithophore concentrations occurred in late winter and spring, and low densities occurred in the summer and fall. The high coccolithophore densities during spring 1992 were associated with unusually low surface nutrient concentrations and a lack of upwelling, suggesting that the high densities were not part of a typical spring phytoplankton bloom in this region. We propose that the suppression of upwelling during spring 1992 may have been related to the prevailing ENSO conditions. Emiliania huxleyi type A dominated the total coccolithophore population throughout the year, Umbilicosphaera sibogae var. sibogae being the second most important contributor to the coccolithophore assemblages.  相似文献   
994.
A simple shaker table for seismometer calibration   总被引:1,自引:0,他引:1  
A unique and simple shaker table (shake table or shaking table), designed, constructed, and installed at the Hawaii Institute of Geophysics, has proven to be a valuable aid in testing and calibrating short period seismometers, as well as ocean bottom and ocean sub-bottom seismometer/tilt meter packages. It consists of a platform suspended in a stairwell by a single elastic cord (10 m extended length) driven by GeoSpace HS-10 geophones. Platform motion is monitored by orthogonal reference geophones and tilt meters. The relatively low natural periods of the platform, about 1.9 sec vertical and 6.5 sec horizontal, provide sufficient isolation from local vibrations that calibration can be made near operational amplitudes. Vertical or horizontal driver geophones can be driven by a commercial signal generator or white noise generator, or from magnetic tape output. The table can also be tilted with respect to the drivers to determine tilt tolerances and to calibrate tilt meters. A Hewlett-Packard 3582-A spectrum analyzer, used to analyze both reference and output signals, provides near real-time system cabibration and is an efficient means for investigating parasitic system resonances. The analyzer can also provide a white noise signal source to the driver geophones.Hawaii Institute of Geophysics Contribution 1443.  相似文献   
995.
996.
The validity of analyses of elements in the femto- and picomolar ranges in waters and sediments can be assessed on the basis of several criteria: an evaluation of the chemical technique; the use of primary standards and intercalibration exercises; and chemical and geochemical coherence of the results. Herein are reported analyses of ruthenium, platinum, palladium, rhenium, iridium and gold in oceanic samples. The gold concentrations in surface seawaters, at least 25 times less than those previously reported, are in accord with the concentrations of their periodic table neighbors as well as with crustal and sedimentary contents. The remarkable concentration of rhenium in seawater, in relation to its very low crustal abundance, can be explained by the inertness of the perrhenate ion.  相似文献   
997.
998.
999.
1000.
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