全文获取类型
收费全文 | 7443篇 |
免费 | 1243篇 |
国内免费 | 1326篇 |
专业分类
测绘学 | 2467篇 |
大气科学 | 719篇 |
地球物理 | 1546篇 |
地质学 | 3142篇 |
海洋学 | 709篇 |
天文学 | 369篇 |
综合类 | 525篇 |
自然地理 | 535篇 |
出版年
2024年 | 24篇 |
2023年 | 68篇 |
2022年 | 271篇 |
2021年 | 333篇 |
2020年 | 336篇 |
2019年 | 355篇 |
2018年 | 278篇 |
2017年 | 414篇 |
2016年 | 393篇 |
2015年 | 380篇 |
2014年 | 520篇 |
2013年 | 554篇 |
2012年 | 530篇 |
2011年 | 522篇 |
2010年 | 397篇 |
2009年 | 479篇 |
2008年 | 527篇 |
2007年 | 479篇 |
2006年 | 495篇 |
2005年 | 455篇 |
2004年 | 388篇 |
2003年 | 272篇 |
2002年 | 294篇 |
2001年 | 207篇 |
2000年 | 181篇 |
1999年 | 154篇 |
1998年 | 138篇 |
1997年 | 108篇 |
1996年 | 74篇 |
1995年 | 71篇 |
1994年 | 73篇 |
1993年 | 64篇 |
1992年 | 47篇 |
1991年 | 32篇 |
1990年 | 29篇 |
1989年 | 13篇 |
1988年 | 19篇 |
1987年 | 7篇 |
1986年 | 6篇 |
1985年 | 2篇 |
1984年 | 3篇 |
1983年 | 2篇 |
1979年 | 4篇 |
1977年 | 1篇 |
1974年 | 1篇 |
1971年 | 1篇 |
1954年 | 3篇 |
1900年 | 3篇 |
1897年 | 1篇 |
1880年 | 1篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
161.
Masao Komazawa Hitoshi Morikawa Kajuro Nakamura Junpei Akamatsu Keiichi Nishimura Sumio Sawada Ayfer Erken Akin Onalp 《Soil Dynamics and Earthquake Engineering》2002,22(9-12):829-836
The 1999 Kocaeli earthquake brought serious damage to downtown of Adapazari. To study why strong motions were generated at the town, a bedrock structure was investigated on the basis of Bouguer gravity anomaly, and SPAC and H/V analyses of microseisms. It was revealed that, the basin consists of three narrow depressions of bedrock with very steep edges, extending in E–W or NE–SW directions along the North Anatolia faults, and the depth to bedrock reaches 1000 m or more. Downtown of Adapazari is located 1–2 km apart from the basin-edge. It is considered that, the specific configuration of bedrock amplifies ground motions at the downtown area by focusing of seismic waves and/or interference between incident S-waves and surface-waves secondarily generated at the basin-edge. Studying 3D bedrock structure is an urgent issue for microzoning an urban area in a sedimentary basin. 相似文献
162.
Pierre Hudon In-Ho Jung Don R. Baker 《Physics of the Earth and Planetary Interiors》2002,130(3-4):159-174
Melting relations of β-quartz were experimentally determined at 1.0 GPa (1900±20 °C), 1.5 GPa (2033±20 °C), and 2.0 GPa (2145±20 °C) using a new high-pressure assembly in a piston–cylinder apparatus and substantial differences were found with data previously reported. The new melting data of β-quartz were combined and optimized with all available thermodynamic, volumetric, and phase equilibria data for β-cristobalite, β-quartz and coesite to produce a P–T liquidus diagram for silica valid up to 6.0 GPa. Using the new optimized thermodynamic parameters, the invariant point β-cristobalite+β-quartz+liquid and β-quartz+coesite+liquid were determined to lie at 1687±17 °C and 0.457 GPa, and 2425±25 °C and 5.00 GPa, respectively. 相似文献
163.
Chen Po-fang 《地震学报(英文版)》2002,15(5):519-525
To improve the accuracy of the numerical evaluation through the 3-D finite difference method, the surface boundary conditions
are added to modify the old program. The author has tested the new program by making calculations for the model constructed
by Wanamaker, et al (1984). The comparison between the numerical results obtained from this paper and those by Wannamaker, et al (1984) indicates that a pronounced improvement is realized in the evaluation of the horizontal magnetic components. Moreover,
better calculations for the vertical magnetic components are also obtainable by using the new program. 相似文献
164.
165.
166.
Fe‐rich metapelitic granulites of the Musgrave Block, central Australia, contain several symplectic and coronal reaction textures that post‐date a peak S2 metamorphic assemblage involving garnet, sillimanite, spinel, ilmenite, K‐feldspar and quartz. The earliest reaction textures involve spinel‐ and quartz‐bearing symplectites that enclose garnet and to a lesser extent sillimanite. The symplectic spinel and quartz are in places separated by later garnet and/or sillimanite coronas. The metamorphic effects of a later, D3, event are restricted to zones of moderate to high strain where a metamorphic assemblage of garnet, sillimanite, K‐feldspar, magnetite, ilmenite, quartz and biotite is preserved. Quantitative mineral equilibria calculations in the system K2O–FeO–MgO–Al2O3–SiO2–H2O–TiO2–Fe2O3 (KFMASHTO) using Thermocalc 3.0 and the accompanying internally consistent dataset provide important constraints on the influence of TiO2 and Fe2O3 on biotite‐bearing and spinel‐bearing equilibria, respectively. Biotite‐bearing equilibria are shifted to higher temperatures and spinel‐bearing equilibria to higher pressures and lower temperatures in comparison to the equivalent equilibria in K2O–FeO–MgO–Al2O3–SiO2–H2O (KFMASH). The sequence of reaction textures involving spinel is consistent with a D2 P–T path that involved a small amount of decompression followed predominantly by cooling within a single mineral assemblage stability field. Thus, the reaction textures reflect changes in modal proportions within an equilibrium assemblage rather than the crossing of a univariant reaction. The D3 metamorphic assemblage is consistent with lower temperatures than those inferred for D2. 相似文献
167.
168.
169.
170.
影像匹配技术在图像处理与计算机视觉中有着非常重要的作用。最小二乘影像匹配方法是常用的匹配方法之一。本文简单介绍了目前影像匹配的几种方法及其优缺点,探讨了数字相机的检校原理与方法。重点介绍附有约束条件的最小二乘影像匹配的原理及匹配过程,结合交通事故处理的实例,论证了该方法的可行性。与传统方法相比,在测量精度、自动化程度以及数据三维可视化等方面具有明显优势。 相似文献