全文获取类型
收费全文 | 5519篇 |
免费 | 857篇 |
国内免费 | 1593篇 |
专业分类
测绘学 | 1528篇 |
大气科学 | 437篇 |
地球物理 | 882篇 |
地质学 | 3081篇 |
海洋学 | 940篇 |
天文学 | 328篇 |
综合类 | 343篇 |
自然地理 | 430篇 |
出版年
2024年 | 83篇 |
2023年 | 246篇 |
2022年 | 265篇 |
2021年 | 285篇 |
2020年 | 237篇 |
2019年 | 325篇 |
2018年 | 235篇 |
2017年 | 255篇 |
2016年 | 236篇 |
2015年 | 296篇 |
2014年 | 422篇 |
2013年 | 285篇 |
2012年 | 352篇 |
2011年 | 330篇 |
2010年 | 367篇 |
2009年 | 353篇 |
2008年 | 315篇 |
2007年 | 322篇 |
2006年 | 305篇 |
2005年 | 286篇 |
2004年 | 260篇 |
2003年 | 235篇 |
2002年 | 187篇 |
2001年 | 194篇 |
2000年 | 150篇 |
1999年 | 120篇 |
1998年 | 108篇 |
1997年 | 120篇 |
1996年 | 128篇 |
1995年 | 104篇 |
1994年 | 84篇 |
1993年 | 72篇 |
1992年 | 93篇 |
1991年 | 68篇 |
1990年 | 68篇 |
1989年 | 64篇 |
1988年 | 16篇 |
1987年 | 10篇 |
1986年 | 12篇 |
1985年 | 8篇 |
1984年 | 7篇 |
1982年 | 9篇 |
1981年 | 3篇 |
1980年 | 9篇 |
1979年 | 5篇 |
1977年 | 4篇 |
1965年 | 4篇 |
1964年 | 4篇 |
1957年 | 5篇 |
1954年 | 4篇 |
排序方式: 共有7969条查询结果,搜索用时 15 毫秒
151.
利用频谱解混叠方法实现超分辨率影像重建 总被引:3,自引:0,他引:3
基于信号处理的超分辨率影像重建技术,可以消除由影像系统引起的影像模糊和退化,同时恢复出光学权限外的频谱信息。首先简要介绍了超分辨率影像重建技术的意义和基本过程;并对影像配准与运动模型估计在超分辨率影像重建中的作用给予简要介绍;接着根据连续傅里叶变换(CFT)和离散傅里叶变换(DFT)的频谱混叠关系及CFT位移性质,推导出频谱解混叠的超分辨率影像重建模型;最后采用文献中的运动模型估计方法和本文的重建算法,对几组数据进行实验,获得了空间分辨率提高近1倍的影像。 相似文献
152.
153.
利用拉曼光谱学和费氏台方法对若干地区超高压榴辉岩中柯石英和榴辉岩中石英出溶体的超显微构造特征进行了研究。研究结果表明,石榴石(或绿辉石)中柯石英向石英相变是一个连续变化过程。绿辉石中石英出溶体和主晶具有一定的晶体学拓扑关系,即石英出溶体长轴有两个展布方向:平行于绿辉石(100)裂理面和平行于绿辉石(-101)面。目前,部分学者推断榴辉岩绿辉石中石英出溶体可作为超高压变质作用的标志。笔者认为,棒状定向石英在绿辉石中出溶的温压条件和出溶机理尚未查明。因此,需加强过量二氧化硅单斜辉石出溶机理的超高压实验研究,从而为证实石英出溶体作为超高压标志提供实验定量约束。 相似文献
154.
本文以杭州湾大桥工程为重点试图对杭州湾地区浅层天然气在杭州湾地区的形成、分布特征作一概括,分析了浅层气喷发对土层及工程基础产生负摩阻力、沉降等危害,从浅层气的成因机制上找出工程施工中解决浅层天然气的对策(控制性释放)。 相似文献
155.
ZHANGJin MAZongjin RENWenjun LEIYongliang 《大地构造与成矿学(英文版)》2003,27(1):165-178
There are many thrust-related structures occurring in the Paleozoic strata of the Niushou Mountain in the central part of Ningxia Hui Autonomous Region. The fault-related folds are the typical structures in this area. Based on the analysis about these structures and their relationships, the processes by which these structures of the Miboshan Formation were formed are reconstructed, and the strata underwent about three stages of deformation: (1) horizontal shortening, (2) folding, and (3) thrusting. And the fact that the Niushou Mountain is the leading edge of an old thrust sheet was proved, the Niushou Mountain, the Daluo Mountain and the Xiaoluo Mountain together constitute the front part of this old thrust zone, so the Niushou Mountain and the Ordovician strata in the central and southern parts of Ningxia now are likely allochthons. In the period from middle Ordovician to Devonian, the areas of the central and southern Ningxia belonged to the back-arc foreland basin of North Qilianshan orogen, which was adjacent to the continent in the north. In the later part of the early Paleozoic period, the Niushou Mountain was formed after the closure of the back-arc foreland basin. 相似文献
156.
ZHUWenbin MARuishi GUOLingzhi SUNYan XUMingjie HUDezhao 《大地构造与成矿学(英文版)》2003,27(1):179-190
The central structure belt in Turpan-Hami basin is composed of the Huoyanshan structure and Qiketai structure formed in late Triassic-early Jurassic, and is characterized by extensional tectonics. The thickness of strata in the hanging wall of the growth fault is obviously larger than that in the footwall, and a deposition center was evolved in the Taibei sag where the hanging wall of the fault is located. In late Jurassic the collision between Lhasa block and Eurasia continent resulted in the transformation of the Turpan-Hami basin from an extensional structure into a compressional structure, and consequently in the tectonic inversion of the central structure belt of the Turpan-Hami basin from the extensional normal fault in the earlier stage to the compressive thrust fault in the later stage. The Tertiary collision between the Indian plate and the Eurasian plate occurred around 55Ma, and this Himalayan orogenic event has played a profound role in shaping the Tianshan area, only the effect of the collision to this area was delayed since it culminated here approximately in late Oligocene-early Miocene. The central structure belt was strongly deformed and thrusted above the ground as a result of this tectonic event. 相似文献
157.
通过在水布垭水利枢纽地下厂房中进行变形试验,研究了厂房区岩体的变形特性,采用反分析法进行粘弹性反分析,反演出地应力、弹性模量及粘性参数,并与现场试验结果进行比较,对反算值进行评价。 相似文献
158.
159.
Fractal and Multifractal Modeling of Hydrothermal Mineral Deposit Spectrum: Application to Gold Deposits in Abitibi Area, Ontario, Canada 总被引:2,自引:0,他引:2
ChengQiuming 《中国地质大学学报(英文版)》2003,14(3):199-206
A number of fractal/multifractal methods are introduced for quantifying the mineral de-lmsit spectrum which include a number-size, grade-tonnage model, power spectrmn model,multi-fractal model and an eigeavalue spectrmn model The first two models characterize mineral deposits spec-tra based on relationships among the measures of mineral deposits.These include the number of deposits,size of deposits,concentration and volume of mineral deposits.The last three methods that deal with the spatial-temporal spectra of mineral deposit studies are all expected to be popularized in near future.A case study of hydrothermal gold deposits from the Abitibi area,a world-class mineral district is used to demonstrate the principle as well as the applications of methods proposed in this paper,It has been shown that fractal and multifractal models are generally applicable to modeling of mineral deposits and occurrences.Clusters of mineral deposits were identified by several methods including the power spectral eral deposits in the Timmins and Kirkland Lake camps. 相似文献
160.