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51.
The buried Chicxulub impact structure is marked by a dramatic ring of sinkholes (called cenotes if containing water), and adjacent less prominent partial rings, which have been shown to coincide with maxima in horizontal gravity gradients and a topographic depression. These observations, along with the discreteness and spacing of the features, suggest a formation mechanism involving faulting in the outer slump zone of the crater, which would thus have a diameter of approximately 180 km.
An opposing view, based primarily on the interpretation of gravity data, is that (he crater is much larger than the cenote ring implies. Given the association of the known cenote ring with faults, we here examine northern Yucatan for similar rings in gravity, surface features and elevation, which we might expect to be associated with outer concentric faults in the case of a larger, possibly multiring, structure.
No such outer rings have been found, although definite patterns are seen in the distribution of karst features outside the crater rim. We explain these patterns as resulting mainly from deformation related to the block fault zone that parallels tbe shelf edge of eastern Yucatan.  相似文献   
52.
发生在沉积物-水界面的剧烈生物地球化学作用对沉积物和上覆水体具重要的环境效应,然而此方面研究很少。本文通过云贵高原四个湖泊湖水和孔隙水NH和NO剖面,沉积物柱芯不同结合态氮含量剖面分布,界面扩散通量,影响氮循环的因素及它们季节性变化规律等的对比研究,初步揭示了湖泊沉积物一水界面的氮循环及其环境效应。  相似文献   
53.
从液动锤基础理论出发,依据理论计算公,科学建立数学模型,开发计算机软件,对液动锤内部动力过程及工作参数进行计算机模拟仿真电算,寻求大幅度提高冲击功的途径和方法。  相似文献   
54.
试论温室效应对我国西部河川径流的影响   总被引:2,自引:1,他引:2  
赖祖铭 《冰川冻土》1997,19(1):10-16
大气中日益增多的温室气体使我国西部地区的气候近三四十年来出现了干暖化趋势,导致河川径流量明显减少。据统计,从50年代后半期到80年代,新疆地区的河种径流量减少了6.4%,西藏东南部的3条大河从60年代到80年代则平均减少了13.2%,其减少量大于新疆,这主要是因为气温升高使冰雪融水增加,新疆的河流受到冰雪融水的补偿,虽然西藏东南部的河注也有冰川存在,甚至冰种覆盖面积远大于新疆一些内陆河流域,但那里  相似文献   
55.
Introduction With rapid development and advancement of economy and society, lots of city groups or city belts with ex-tra-large cities as their centers have been formed in China. The regions these city groups lie in usually have well-developed economy, dense population, and are regional politics and culture centers. Some groups lie in the regions with high level of earthquake activity, such as the Surrounding Capital City Group with the centers of Bei-jing and Tianjin. Once a large earthqua…  相似文献   
56.
Geologic marks related to extraterrestrial impact events, such as impact split gravels, impact brecciate layers, impact dikes, microirghizites, microtektites, especially meteoritic residues, were discovered on the boundary between Sinian/Cambrian at Tianmenshan of Western Hunan, which may possibly demonstrate that an extraterrestrial impact event has ever occurred there on the S/C boundary.  相似文献   
57.
矿产资源规划环境影响评价工作方法探讨   总被引:10,自引:0,他引:10  
李善峰  张进德 《地质通报》2004,23(11):1153-1156
根据《中华人民共和国环境影响评价法》关于规划的环境影响评价要求,初步探讨了矿产资源规划环境影响评价的工作思路。参照国土资源部《矿产资源规划管理暂行办法》的有关规定,列举了矿产资源规划的类型;依据《环评法》第七条和第八条,阐明了不同类型的矿产资源规划所对应的环境影响评价文件编制的要求;提出了矿产资源规划环境影响评价的工作程序和环境影响评价指标体系的建议,并简单地探讨了2种评价方法。  相似文献   
58.
Large volumes of mare basalts are present on the surface of the moon, located preferentially in large impact basins. Mechanisms relating impact basins and mare basalt eruptions have previously been suggested: lunar impacts removed low-density material that may have inhibited eruption, and created cracks for fluid flow [Icarus 139 (1999) 246], and lunar basins have long been described as catchments for magma (e.g., [Rev. Geophys. Space Phys. 18 (1980) 107] and references therein). We present a new model for melt creation under near side lunar basins that is triggered by the impacts themselves. Magma can be produced in two stages. First, crater excavation depressurizes underlying material such that it may melt in-situ. Second, the cratered lithosphere rises isostatically, warping isotherms at the lithosphere-asthenosphere boundary which may initiate convection, in which adiabatic melting can occur. The first stage produces by far the largest volume of melt, but convective melting can continue for up to 350 Ma. We propose that giant impacts account for a large portion of the volume and longevity of mare basalt volcanism, as well as for several compositional groups, including high alumina, high titanium, KREEP-rich, and picritic magmas.  相似文献   
59.
The process of crater formation by the impact of water drops on soil, sand and various other target material was studied. Craters of various shapes and sizes were observed on different target materials or conditions, ranging from circumferential depression to completely hemispherical shape. Crater shape was dependent upon target material, its ?ow stress or shear strength and the presence and thickness of water on the surface. Between 5 and 22 per cent of impact energy was spent on cratering, but the relationship between crater volume and kinetic energy of a raindrop was curvilinear, indicating a lower ef?ciency of impact energy in removing target material as the energy increases. Impact impulse, on the other hand, showed a more linear relationship with crater volume, and the ratio of impulse over crater volume (I/V) remained constant for the entire range of drop sizes, impact velocities, and surface conditions used in this study. Surface shear strength, represented by the penetration depth of fall‐cone penetrometer, appeared to be a key factor involved in this process. An equation was developed which related crater volume to cone penetration depth and impact impulse. Crater volume, which appeared to be a better indicator of the total amount of material dislodged by a raindrop than splash amount, can thus be predicted using this equation. Copyright © 2004 John Wiley & Sons, Ltd.  相似文献   
60.
Introduction Through many year's practices by vast numbers of scientific and technological workers andefforts from all aspects, the dynamic testing method of high-low strain has formally entered intothe technical code of foundation pile test of construction at last (The Industry Standards of thePeople's Republic of China, 2003). The striking mode of the dynamic testing method of high strainis stipulated as hammer in the code, the striking of rocket can also be used. The latter is widely…  相似文献   
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