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   18781篇
  免费   2820篇
  国内免费   4553篇
测绘学   637篇
大气科学   1475篇
地球物理   3406篇
地质学   10487篇
海洋学   1684篇
天文学   5209篇
综合类   984篇
自然地理   2272篇
  2024年   86篇
  2023年   265篇
  2022年   628篇
  2021年   633篇
  2020年   627篇
  2019年   792篇
  2018年   659篇
  2017年   577篇
  2016年   630篇
  2015年   761篇
  2014年   1021篇
  2013年   1054篇
  2012年   1199篇
  2011年   1236篇
  2010年   1273篇
  2009年   1637篇
  2008年   1504篇
  2007年   1475篇
  2006年   1410篇
  2005年   1214篇
  2004年   1111篇
  2003年   920篇
  2002年   825篇
  2001年   744篇
  2000年   655篇
  1999年   623篇
  1998年   513篇
  1997年   333篇
  1996年   308篇
  1995年   258篇
  1994年   240篇
  1993年   228篇
  1992年   158篇
  1991年   96篇
  1990年   90篇
  1989年   73篇
  1988年   66篇
  1987年   34篇
  1986年   37篇
  1985年   37篇
  1984年   23篇
  1983年   18篇
  1982年   17篇
  1981年   7篇
  1980年   15篇
  1979年   9篇
  1978年   6篇
  1977年   16篇
  1954年   7篇
  1875年   1篇
排序方式: 共有10000条查询结果,搜索用时 31 毫秒
81.
82.
83.
Summary. A residual map of the total magnetic field (above 25 000 nT base) is presented for a portion of the central crystalline shield area of Nigeria and overlapping small portions of the Chad basin and the Benue rift (8°30'−12° 00'lat, and 7°−10°30' long). The map (based on a dataset digitized from recently released aeromagnetic sheets of Nigeria) leads to four results. (1) A magnetic boundary, evident on the map, separates the Younger Granite complexes into two groups. The groups are petrologically different, and the boundary may be a fault line with uplift to the south. (2) South of the boundary the map is dominated by a system of sub-parallel anomalies striking NE–SW, possibly representing major tectonic trends, and a set of fractures through which the Younger Granite complexes were intruded. The trend of the system parallels the Benue rift and lineaments in the oceanic crust off West Africa. (3) Negative magnetic anomalies lie over most of the known ring complexes, and over some suspected buried ring complexes and other intrusions. (4) 2½-and 3-D modelling shows that the larger complexes extend to 12 km depth, and the smaller ones to 6 km. They have nearly vertical sides, and magnetization contrasts range from 0.3 to 0.5 A m−1.  相似文献   
84.
Photoelectric radial-velocity measurements show that HD 118670 is a double-lined spectroscopic binary in an orbit which is not quite circular and whose period is about 48 days. Spectral types of K0 V and K7 V would satisfy the photometry and the mass ratio; the mass function would then suggest the possibility of eclipses. However, actual spectral classification indicates a luminosity somewhat above the main sequence  相似文献   
85.
86.
87.
88.
89.
90.
We analyse the non-linear, three-dimensional response of a gaseous, viscous protoplanetary disc to the presence of a planet of mass ranging from 1 Earth mass (1 M) to 1 Jupiter mass (1 MJ) by using the zeus hydrodynamics code. We determine the gas flow pattern, and the accretion and migration rates of the planet. The planet is assumed to be in a fixed circular orbit about the central star. It is also assumed to be able to accrete gas without expansion on the scale of its Roche radius. Only planets with masses   M p≳ 0.1 MJ  produce significant perturbations in the surface density of the disc. The flow within the Roche lobe of the planet is fully three-dimensional. Gas streams generally enter the Roche lobe close to the disc mid-plane, but produce much weaker shocks than the streams in two-dimensional models. The streams supply material to a circumplanetary disc that rotates in the same sense as the orbit of the planet. Much of the mass supply to the circumplanetary disc comes from non-coplanar flow. The accretion rate peaks with a planet mass of approximately 0.1 MJ and is highly efficient, occurring at the local viscous rate. The migration time-scales for planets of mass less than 0.1 MJ, based on torques from disc material outside the Roche lobes of the planets, are in excellent agreement with the linear theory of type I (non-gap) migration for three-dimensional discs. The transition from type I to type II (gap) migration is smooth, with changes in migration times of about a factor of 2. Starting with a core which can undergo runaway growth, a planet can gain up to a few MJ with little migration. Planets with final masses of the order of 10 MJ would undergo large migration, which makes formation and survival difficult.  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