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   17317篇
  免费   1947篇
  国内免费   3774篇
测绘学   2010篇
大气科学   2946篇
地球物理   1782篇
地质学   6428篇
海洋学   1793篇
天文学   5625篇
综合类   936篇
自然地理   1518篇
  2024年   69篇
  2023年   205篇
  2022年   495篇
  2021年   580篇
  2020年   620篇
  2019年   758篇
  2018年   509篇
  2017年   597篇
  2016年   615篇
  2015年   679篇
  2014年   986篇
  2013年   1053篇
  2012年   1070篇
  2011年   1152篇
  2010年   1126篇
  2009年   1515篇
  2008年   1424篇
  2007年   1398篇
  2006年   1273篇
  2005年   1063篇
  2004年   967篇
  2003年   789篇
  2002年   641篇
  2001年   591篇
  2000年   535篇
  1999年   499篇
  1998年   372篇
  1997年   228篇
  1996年   189篇
  1995年   158篇
  1994年   146篇
  1993年   161篇
  1992年   84篇
  1991年   72篇
  1990年   69篇
  1989年   65篇
  1988年   48篇
  1987年   23篇
  1986年   36篇
  1985年   37篇
  1984年   31篇
  1983年   19篇
  1982年   16篇
  1981年   7篇
  1980年   18篇
  1979年   5篇
  1978年   7篇
  1977年   17篇
  1976年   4篇
  1973年   7篇
排序方式: 共有10000条查询结果,搜索用时 35 毫秒
971.
笔者通过对澜沧某电站右岸坝肩复杂岩体的成因进行分析,采用岩体质量指数Z并结合水利水电工程围岩分级和RMR分级等岩体分类方法对电站右岸坝肩的复杂岩体进行了综合分类。  相似文献   
972.
The application of the ground penetrating radar (GPR) at two archaeological sites, Serrano and Morro Grande, situated in Araruama County, Rio de Janeiro, Brazil, aids the study of a prehistoric indigenous culture, associated with the “Tupinambá” that inhabited the region during prehistoric times.The archaeological remains of the study area are mainly characterized by pottery artifacts for several uses, including funerary urns, which were buried within layers of sand and clay. Several profiles were acquired using a RAMAC system, with a 200 and 400 MHz frequency antennae. At the Serrano site, the profiles were acquired around some partially exposed pottery shards, due to sand exploitation. The resultant profiles provided a response model to guide the interpretation of new profiles acquired at other sites in the area, which present similar characteristics.The results showed the great importance of the dielectric permittivity contrast which exists between the targets and the host media, in order for possibly significant features to be identified in radar data.  相似文献   
973.
Broadband synthetic aperture borehole radar interferometry   总被引:1,自引:0,他引:1  
Trials in mines have established that wideband VHF borehole radars (BHR), working in the 10–100-MHz band, can be used to probe the rockmass between boreholes over ranges from <5 m to as much as 150 m with submeter resolution. There is evidence that ore bodies reflect these radar signals both specularly and diffusely, much as the ground/air interface does when overflown by synthetic aperture radar (SAR). In both SAR and BHR, multiple flight lines, together with diffuse reflections admit the possibility of developing interferometric 3D images of the object. This paper examines the possibility of imaging buried objects in three dimensions by interferometrically combining broadband VHF borehole radar profiles shot in adjacent pairs of boreholes. Broadbanding in BHR has the advantage of releasing the image from 2 phase ambiguities, but practically, interferometric borehole radar (InBHR) needs high signal-to-noise ratios (SNR) to avoid noise capture. This means that 3D InBHR is limited to ranges in wavelengths which are less than the rock's attenuation factor Q. Interferometric methods are developed which are capable of mapping ore bodies and other structures in three dimensions. Tangent plane migration methods are developed here in order to reconstruct surfaces that lie in the near-field of sparse interferometric arrays.  相似文献   
974.
The numerical algorithm of calculation of Lyapounov coefficients (L k) of any order is developed. The apparatus of analytical calculations is not used in this algorithm. The proposed algorithm is of use for usual computer languages and allows us to find the numerical value of L k for any k and to make complete qualitative analyses of dynamic models on the plane.  相似文献   
975.
A carbonate-hosted stratabound siliceous crust type (SCT) mineralization (base metal sulphides, barite, fluorite) occurs over large areas of Carnic Alps and Karawanken in the Eastern Alps. It concerns a pervasively silicified lithological unit, up to some tens of metres thick, which caps the unconformity landscapes developed on epicontinental Devonian–Dinantian carbonates. The SCT mineralization is directly overlaid by different transgressive siliciclastic sediments, which range from Lower Carboniferous to Lower Permian. The presence of fragments of the SCT mineralization in the transgressive siliciclastic sediment bounds its whole lithological evolution within a short stratigraphic interval of Lower Carboniferous age. Selected features of the regional and lithostratigraphic setting are discussed. The chemical characterisation is based on the statistical evaluation of compositional data of 581 selected samples. Three significant groups of elements have been distinguished: (1) the hydrological and metasomatically active elements (Si, Ba, F), which show a strong negative correlation amongst themselves and characterise the silica-saturated aqueous solutions; (2) the terrigenous elements (Al2O3, K2O, Fetot, TiO2, B, Be, Ce, La, Nb, V, Y, Zr), which suggest a continental margin environment for silica deposition; (3) the sulphide metals (Cu, Pb, Zn, Ni, Sb, As, Hg, Cd), which define the metalliferous signature of the SCT mineralization.Some consistent, but still debatable genetic aspects of the SCT mineralization are as follow: (1) silica may be supplied by illitization of clay-rich basinal sediments during their diagenesis. δ18O of microcrystalline quartz ranges from +18.5‰ and +24.6‰ and is very similar to δ18O of authigenic quartz deriving from diagenetic processes of illitization of clay-rich basinal sequences. (2) The diagenetic evolution of these sediments may trigger off the movement of silica-rich marine pore waters. δ34S of barite ranges from +15.5‰ to +19.3‰ with an average of +17.7‰ and are in good agreement with δ34S of sulphate in ocean waters of Upper Devonian–Lower Carboniferous age. (3) A convective hydrological system, connected with sinsedimentary transtensive tectonics, active in the Carnic Alps since the Frasnian, may be the transport mechanism of aqueous solutions. (4) A weak drop in pH in the dominant carbonate environment represents the conditions for silica precipitation.SCT mineralization, showing persistent, independent and distinct characters, occurs over large areas also in other sites of the Alpine belt and outside Italy and Austria. Therefore, it points to important markers for some sedimentary sequences as well as to a worldwide significant cyclic metallogenic event. It represents a new ore deposit-type within the carbonate-hosted mineralization.  相似文献   
976.
Short-wave infrared reflectance spectra obtained from a Portable Infrared Mineral Analyser (PIMA) have been used to define alteration zones adjacent to base metal sulfide ore bodies at the Elura Mine, Cobar, Australia. The spectroscopic work identified white mica (sericite), chlorite and carbonates of hydrothermal origin in the alteration zones associated with the ore bodies. Weathering, alteration and ore zones can be discriminated by variations in the intensity and wavelength of relevant absorption features. Hydrothermal alteration is classified into four principal types, namely sericitic, silicic, chloritic and carbonate alteration. The first three types comprise overprinting hydrothermal assemblages of quartz, sericite, chlorite, ankerite, siderite, calcite and sulfides developed in strongly altered metasiltstone and slate of Early Devonian age, adjacent to the zinc–lead–silver mineralisation. An extensive zone of carbonate alteration, manifested as porphyroblasts of siderite in the host metasediments, is recognised beyond the zones of strong alteration. Spectral analysis is consistent with the mineralogical data obtained from XRD and XRF analyses and defines the limits of the alteration zones to distances of about 80 m around the ore bodies. The study demonstrates the potential for spectral analysis to assist with drill hole logging and the identification of alteration zones as part of mineral exploration and development programs.  相似文献   
977.
杨修群  谢倩 《气象学报》1996,54(1):42-52
利用发展的包含海洋表面边界展和大气辐合反馈过程的热带太平洋海气耦合距平模式,对ENSO循环进行了模拟。通过30a积分,用合模式所展示的热带太平洋海气耦合系统的ENSO循环的水平结构演变特征和观测事实甚为一致,成功地模拟出了ENSO循环的冷暖态的发生发展、衰亡及相互转换等各个位相的动力和热力场的水平结构及其对季节循环的依赖性特征。本文数值模拟结果表明,ENSO循环的主要动力学过程可由热带海气相互作用系统自身所确定。ENSO循环的正确模拟是揭示其形成机制的前提。  相似文献   
978.
杨修群  谢倩 《气象学报》1996,54(6):719-721
利用热带太平洋海气耦合异常模式的30a模拟结果,对模式ENSO的变化性及多重时间尺度过程进行了细致分析,建立了一ENSO循环多重时间尺度过程相互作用的非线性相似(Analog)模型,并提出了ENSO循环主周期形成的一种可能机制。指出:和观测事实类似,模式ENSO过程确实涉及到三种时间尺度,即3—4a主周期振荡(LF)、准两年振荡(QB)和年循环(AC);其中,QB过程是线性海气耦合系统的本征模态,年循环(AC)对其形成没有本质的影响;3—4a主周期振荡(LF)是一非线性系统的自激振荡现象,其形成是线性系统的本征模即QB过程通过非线性机制尤其是通过大气辐合反馈加热的“单向性”过程在QB的暖态产生的减频增幅所致;平均年循环(AC)虽然不能对ENSO循环形成有本质影响,但它可明显影响ENSO循环的具体振幅和位相,使得ENSO循环具有明显的不规则性并对季节循环具有明显的“锁相”特征;ENSO变化性确是LF、QB以及AC多重时间尺度相互作用形成的。本文提出的ENSO循环时间尺度选择机制不仅解释了主周期振荡的形成过程,而且也较好地解释了ENSO变化的谱,因此,这一机制更接近于观测事实。  相似文献   
979.
利用水汽图象分析中尺度云团   总被引:2,自引:0,他引:2  
郑新江  李献洲 《气象》1996,22(1):42-45
利用NOAA卫星提供的水汽图(6.7μm),配合GMS云图、多普勒雷达照片,分析了中尺度暴雨云团发生的位置、演变及其结构,最后给出了有关方法的预报框图。  相似文献   
980.
针对纹理影像先估计出其马尔可夫随机场参数,后运用多元统计分析中模糊聚类分析的数学方法进行定量分类,从而为解决划分上的不确定性现象找出描述方法,获得客观的分类结果  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