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991.
童小华  叶真  刘世杰 《测绘学报》2017,46(10):1500-1508
卫星平台颤振是高分辨率卫星在轨运行普遍存在的复杂现象,会影响卫星的测图精度和成像质量。本文提出了综合多传感器数据处理的卫星颤振探测与补偿技术方法,根据多光谱影像、三线阵影像、密集地面控制和姿态测量数据进行了颤振探测,采用像方补偿和姿态补偿两种方式进行了颤振补偿。利用本文提出的技术对资源三号卫星的平台颤振问题进行了处理和分析,试验结果验证了所提出的方法用于颤振探测与补偿的有效性与可靠性。颤振变化规律分析表明资源三号卫星颤振的频率保持在0.6~0.7Hz的范围内,而颤振幅值从在轨早期的1个像素下降到0.4个像素以下并趋于平稳。  相似文献   
992.
Urban model retrieval has wide applications in the geoscience field, and it is also a very challenging research topic due to the blur and background clutter in query images and the large spatial inconsistencies between query and database images. In this study, a feature extraction and similarity metric-learning framework for urban model retrieval is proposed. In the method, the selective search voting algorithm is presented to automatically localize and segment a query object from an input image with the help of the top-ranked retrieved database images. Then, the local features of object images are extracted via sparse coding, and the global features are learned using the spatial constrained convolutional neural network. We utilize a new similarity metric to match the database images with a query object image. Finally, similar 3D models are retrieved. Both qualitative and quantitative experimental results indicate that the proposed framework can localize and segment a query object from an input image precisely and that the retrieval results are better than those of other related approaches.  相似文献   
993.
通过断层活动性分析、典型测线平衡剖面恢复、伸展率统计等方法, 对济阳坳陷新生代盆地结构的静态特征和演化过程进行了详细分析, 从凹陷内部结构差异、不同凹陷间结构差异、区域结构差异3个层次上对济阳坳陷盆地进行了对比分析并探讨了成因机制.研究结果表明: 凹陷内部及不同凹陷间结构的差异主要受控于北西向控盆断裂以及不同演化阶段控盆断裂体系的发育, 而区域结构差异主要受控于板块俯冲方式转变下的郯庐断裂带由左旋走滑到右旋走滑的转型以及深部地幔物质由上涌到下沉的转变.  相似文献   
994.
995.
This paper describes a strategy for merging daily precipitation information from gauge observations, satellite estimates(SEs), and numerical predictions at the global scale. The strategy is designed to remove systemic bias and random error from each individual daily precipitation source to produce a better gridded global daily precipitation product through three steps.First, a cumulative distribution function matching procedure is performed to remove systemic bias over gauge-located land areas. Then, the overall biases in SEs and model predictions(MPs) over ocean areas are corrected using a rescaled strategy based on monthly precipitation. Third, an optimal interpolation(OI)–based merging scheme(referred as the HL-OI scheme)is used to combine unbiased gauge observations, SEs, and MPs to reduce random error from each source and to produce a gauge—satellite–model merged daily precipitation analysis, called BMEP-d(Beijing Climate Center Merged Estimation of Precipitation with daily resolution), with complete global coverage. The BMEP-d data from a four-year period(2011–14) demonstrate the ability of the merging strategy to provide global daily precipitation of substantially improved quality.Benefiting from the advantages of the HL-OI scheme for quantitative error estimates, the better source data can obtain more weights during the merging processes. The BMEP-d data exhibit higher consistency with satellite and gauge source data at middle and low latitudes, and with model source data at high latitudes. Overall, independent validations against GPCP-1DD(GPCP one-degree daily) show that the consistencies between BMEP-d and GPCP-1DD are higher than those of each source dataset in terms of spatial pattern, temporal variability, probability distribution, and statistical precipitation events.  相似文献   
996.
Accurately obtaining the structures and damage types of buildings in earthquake stricken areas is fundamental to supporting rescue forces and estimating economic losses and casualties. As the stricken areas are often much larger than the areas covered by very high resolution (VHR) images, the information obtained from VHR images cannot satisfy practical needs. This study developed a method for estimating the structures and types of damaged buildings by combining VHR images, statistics and ground survey data. First, the rates of damaged buildings with different structures and damage types were manually interpreted from VHR images covering a small part of the stricken area, and further corrected by ground survey data. Second, the corrected rates were reallocated to the seismic intensity zones. Third, the rates in the seismic intensity zones and the statistical data were combined to estimate the numbers and areas of damaged buildings in villages, towns and counties. The presented method was applied to estimate the damages caused by the Lushan earthquake in China. The results indicated that our method can efficiently estimate the amount of the damages and complement existing work on only automatic extracting damaged buildings from VHR images.  相似文献   
997.
滩地的淤积层分布记录着以往漫滩洪水的特征,即反映漫滩洪水的量级、频率和持续时间等,同时河漫滩也是预估河流泥沙、洪水灾害防治和湿地生态系统保护等的重要组成部分。根据黄河下游水文年鉴资料,分析滩地的淤积与漫滩洪水的定量关系,为未来河流泥沙预估提供依据。经分析得到大漫滩洪水在来沙系数S/Q<0.030 kg·s/m6时,主槽冲刷而滩地淤积,反之则滩槽同淤。当S/Q<0.030 kg·s/m6时,大漫滩洪水滩地的淤积量主要与漫滩系数Qmax/Qp、上滩水量W0和含沙量S有关;大漫滩洪水的主槽冲刷量则除了与洪水期水量W和沙量Ws有关外,还与滩地的淤积量有关。一般漫滩洪水,当来沙系数S/Q<0.023 kg·s/m6时,主槽冲刷而滩地淤积,反之则滩槽同淤。一般漫滩洪水主槽冲刷量与来沙系数S/Q和洪水期水量W有关,而滩地淤积量仅与含沙量S有关。黄河下游漫滩洪水滩地的淤积和主槽的冲刷主要发生在孙口以上河段,而孙口以下河段主槽冲刷和滩地淤积量均较少。  相似文献   
998.
新疆东准噶尔(东准)构造带晚古生代地层广泛出露,其沉积时限的精确限定对理解该地区及中亚造山带的构造框架具有深远意义。然而东准构造带的地层时代标定存在多种划分方案,分歧较大。依据自测的5个安山岩和9个砂岩的锆石U-Pb年龄以及收集整理的岩浆岩和砂岩的锆石U-Pb年龄约束,认为东准噶尔构造带地质体的形成时代主要在336~268Ma,336Ma地质体沿额尔齐斯、阿尔曼太和卡拉麦里构造带零星分布。原前石炭纪和原石炭纪海相地层主体属于石炭系宾夕法尼亚亚系,部分层段应为同期异相;原石炭纪陆相地层属于二叠系乌拉尔统。东准构造带晚古生代洋盆在晚石炭世同期碰撞拼贴,将其演化阶段分为400~336Ma次生洋盆同期俯冲阶段、336~300Ma洋盆最终闭合消亡阶段、300~270Ma后碰撞伸展阶段及二叠纪中晚期南缘湖相沉积阶段。  相似文献   
999.
1000.
Variations in the mechanical properties (compressive strength, elastic modulus, tensile strength, and fracture toughness) of granite were analyzed as functions of temperature. It was found that above 200 °C, tensile strength and fracture toughness tended to decrease with temperature, while variations in the compressive strength and elastic modulus demonstrated decreasing trends when the heating temperature exceeded 400 °C. The temperature ranges of room temperature—200 and above 600 °C—corresponded to an undamaged state and strongly/completely damaged state, respectively. It is suggested that 400 °C might be a critical threshold of thermal damage to granite. Based on results of statistical tests, a sharp decrease in mechanical properties can be recognized, accompanied by a drastic growth in peaking strain and acoustic emission rate. This phenomenon may be associated with the α/β phase transition of quartz.  相似文献   
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