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   745篇
  免费   207篇
  国内免费   551篇
测绘学   23篇
大气科学   74篇
地球物理   195篇
地质学   928篇
海洋学   138篇
天文学   27篇
综合类   80篇
自然地理   38篇
  2018年   1篇
  2015年   6篇
  2013年   5篇
  2011年   206篇
  2010年   132篇
  2009年   185篇
  2008年   27篇
  2007年   77篇
  2006年   116篇
  2005年   144篇
  2004年   208篇
  2003年   108篇
  2002年   73篇
  2001年   62篇
  2000年   26篇
  1999年   24篇
  1998年   10篇
  1997年   12篇
  1996年   2篇
  1995年   9篇
  1994年   2篇
  1993年   8篇
  1992年   6篇
  1991年   3篇
  1990年   3篇
  1989年   7篇
  1988年   1篇
  1987年   3篇
  1986年   5篇
  1983年   1篇
  1982年   2篇
  1978年   2篇
  1977年   4篇
  1976年   2篇
  1950年   2篇
  1943年   2篇
  1940年   2篇
  1937年   3篇
  1934年   5篇
  1933年   3篇
  1931年   1篇
  1928年   2篇
  1926年   1篇
排序方式: 共有1503条查询结果,搜索用时 15 毫秒
71.
Zircon U-Pb ages and geochemical data of volcanic rocks in the Suifenhe Formation in eastern Heilongjiang Province are reported, and their petrogenesis is discussed in this paper. The Suifenhe Formation mainly consists of basalt, andesite, and dacite. Zircon from andesite and dacite are euhedral in shape and show typical oscillatory zoning with high Th/U ratios (0.18-0.57), implying its magmatic origin. Zircon U-Pb dating results by laser ablation inductively coupled plasma mass spectrometer (LA-ICP-MS) indicate that the 206Pb/238U ages of zircons from andesite range within 105-106 Ma, yielding a weighted mean age of 105.5±0.8 Ma (n=14), and that 206Pb/238U ages of zircons from dacite are between 90-96 Ma, yielding a weighted mean age of 93.2±1.3 Ma (n =13). The volcanic rocks from the Suifenhe Formation are subalkaline series and show a calc-alkaline evolutionary trend with SiO2 content of 47.69%-65.47%, MgO contents of 1.42%-6.80% (Mg#= 45-53), and Na2O/K2O ratios of 1.83-3.63. They are characterized by enrichment in large ion lithophile elements (LILE) and light-rare-earth elements (LREE), depletion in heavy rare earth elements (HREE) and high field strength elements (HFSE) (e.g., Nb, Ta, Ti), and low initial 87Sr/86Sr ratios (0.7041-0.7057) and positiveεNd(t) values (039-4.08), implying that they could be derived from a depleted magma source. Taken together, these results suggest that the primary magma of the volcanic rocks might originate from partial melting of the mantle wedge metasomatized by fluids derived from subducted slab under a tectonic setting of active continental margin.  相似文献   
72.
Secular variations of carbon isotopic composition of organic carbon can be used in the study of global environmental variation, the carbon cycle, stratigraphic delimitation, and biological evolution, etc. Organic carbon isotopic analysis of the Nangao and Zhalagou sections in eastern Guizhou reveals a negative excursion near the Precambrian-Cambrian boundary that correlates with a distinct carbonate carbon isotopic negative excursion at this boundary globally. Our results also demonstrate that several alternating positive and negative shifts occur in the Meishucunian, and an obvious negative anomaly appears at the boundary between the Meishucunian and Qiongzhusian. The isotope values are stable in the middle and lower parts but became more positive in the upper part of the Qiongzhusian. Evolution of organic carbon isotopes from the two sections in the deepwater facies can be well correlated with that of the carbonate carbon isotopes from the section in the shallow water facies. Integrated with other stratigraphic tools, we can precisely establish a lower Cambrian stratigraphic framework from shallow shelf to deep basin of the Yangtze Platform.  相似文献   
73.
In order to study the origin of the spatial structure of the Northern Hemisphere Annular Mode (NAM),a linear stochastic model is constructed empirically from the output of a GCM run.Optimal stochastic forcing in terms of the maximum variance contribution,which may be potentially related to the maintenance of the NAM,is investigated.Theoretical analysis on the dominant non-modal response to the stochastic forcing shows that this dominance is jointly decided by the properties of forcing and the non-modal grow...  相似文献   
74.
A numerical wave flume is constructed based on the Reynolds Averaged Navier-Stokes (RANS) equations with turbulence closure by a modified k-ε model to study the viscous interactions of waves with vertical breakwaters for different overtopping cases. The governing equations,the turbulence model,boundary conditions,and solution method for the numerical wave flume are introduced briefly. The reliability of the numerical wave flume is examined by comparing the numerical results with the experimental measurement...  相似文献   
75.
A total of 34 thunderstorms around Shanghai and Wuhan of China are analyzed in order to determine the relationship between total lightning activity and precipitation particle characteristics.Precipitation particle concentration data are obtained from the 2A12 product of TRMM/TMI(Tropical Rainfall Measuring Mission/TRMM Microwave Image) and lightning activity data are from the TRMM/LIS(Lightning Imaging Sensor) and SAFIR3000(Surveillance et Alerte Founder par Interferometric Radioelectirque).On a spatial ...  相似文献   
76.
A CASE OF MESOSCALE CONVECTIVE COMPLEX EVOLVING INTO A VORTEX   总被引:1,自引:0,他引:1       下载免费PDF全文
A case of mesoscale convective complex(MCC)which evolved into a vortex is documented in this paper.As theMCC entered into the dissipating phase,a well-defined spirally banded structure became visible in the satellite image.The blackbody temperature(TBB)of the residual cold-cloud-shield indicates the vortex existed in the layer from 400 to250 hPa.According to the upper air analysis,the upper level vortex was an anticyclone.The MCC-generated vortex wasvisualized in the satellite images because it was located in the subtropical high where the wind field was very weak.  相似文献   
77.
l. IntroductionGranite distributes widely in western KunlunMts. Many researches have been conducted byscientists (Wang Yuzhen et.al., l987; Zhang Yuquanet.al., l989, Fang Xilian et.al., I990, Jiang Chunfaet.al., 1992; Pan Yusheng, l992, Xu Ronghua et.al.,l 994; Jing Daogui et.al., l996, Zhang Yuquan et.al.,l998). But all of the researches have been donealong Sino-Pakistan road and Xinjiang-Tibet roadt"ith fOcus on isotopic dating of the intrusion andconducted a few on origin and tect…  相似文献   
78.
东昆仑活动断裂带东段古地震活动特征   总被引:12,自引:0,他引:12       下载免费PDF全文
东昆仑活动断裂托索湖——玛曲以东肯定那一带, 可据阿尼玛卿玛积峰为界再分为花石峡段和玛沁段两个在几何上不连续的段落. 两段在表征断层全新世活动特征的古地震事件方面有明显差异, 花石峡段的地震活动性明显高于玛沁段的地震活动性. 古地震研究表明, 花石峡段上3次强震活动相邻两次地震发生的时间间隔分别约为500 a和640 a, 玛沁段上最近两次古地震事件间大致有1 000 a左右的时间间隔. 根据断层平均滑动速率计算的花石峡段7.5级地震的平均复发间隔为411~608 a, 相对应的同震平均水平位错约为(5.75plusmn;0.57)m. 虽然玛沁段的地震活动性较弱, 但由于该段上最近一次地震事件离现在较为久远, 已经积累的应变能应该使我们对其未来地震危险性的分析有足够重视.   相似文献   
79.
中国含油气盆地构造分析主要进展与展望   总被引:4,自引:2,他引:4  
本文简要总结了中国含油气盆地构造分析的主要进展。中国区域大地构造理论特别是板块构造理论,对于指导盆地构造研究起了重要作用。通过各种地球物理探测方法,揭示了中国含油气盆地的上地幔结构,地壳结构、基底结构与盖层构造的关系。中国含油气盆地在地质历史中的演化过程十分复杂,伸展盆地、前陆盆地、走滑盆地、克拉通盆地和叠合具有各自独特的地球动力学系统。构造样式分析是盆地构造分析的重要方面,直接与寻找油气圈闭有关,可以划分出伸展构造、挤压构造、走滑构造、反转构造和潜山-披覆构造等。断裂和不含油气盆地中的重要构造要素,控制着油气运聚成藏、叠合盆地多期成盆、多期改造造成的复杂构成图像,是中国含油气盆地的重要特色之一。展望21世纪 中国油气盆地构造分析,需要重点关注的是:叠合盆地形成演化和地球动力学过程分析;盆-山耦合过程的深部-浅部耦全过程分析;盆地三维构造精细描述和盆地模拟技术,盐构造和天然气构造分析。  相似文献   
80.
This study reports the kinetic experimental results of albite in water and in KCI solution at 22 MPa in the temperature range of 25 to 400℃. Kinetic experiments have been carried out in an open flow-through reaction system (packed bed reactor). Albite dissolution is always incongruent in water at most temperatures, but becomes congruent at 300℃ (close to the critical point 374℃). At temperatures from 25 to 300℃, the incongruent dissolution of albite is reflected by the fact that sodium and aluminum are easily dissolved into water; from 300 to 400℃ it is reflected by silicon being more easily dissolved in water than Al and Na. Maximum albite dissolution rates in the flow hydrothermal systems have been repeatedly observed at 300℃, independent of flow rates.The kinetic experiments of albite dissolution in a KCl aqueous solution (0.1 mol KCl) indicate that the dissolution rate of albite increases with increasing temperature. Maximum silicon release rates of albite have been observed at 400℃, while ma  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