全文获取类型
收费全文 | 2511篇 |
免费 | 557篇 |
国内免费 | 703篇 |
专业分类
测绘学 | 257篇 |
大气科学 | 440篇 |
地球物理 | 637篇 |
地质学 | 1437篇 |
海洋学 | 398篇 |
天文学 | 79篇 |
综合类 | 271篇 |
自然地理 | 252篇 |
出版年
2024年 | 16篇 |
2023年 | 52篇 |
2022年 | 203篇 |
2021年 | 232篇 |
2020年 | 172篇 |
2019年 | 226篇 |
2018年 | 216篇 |
2017年 | 194篇 |
2016年 | 207篇 |
2015年 | 218篇 |
2014年 | 157篇 |
2013年 | 165篇 |
2012年 | 189篇 |
2011年 | 158篇 |
2010年 | 149篇 |
2009年 | 122篇 |
2008年 | 128篇 |
2007年 | 112篇 |
2006年 | 77篇 |
2005年 | 74篇 |
2004年 | 66篇 |
2003年 | 58篇 |
2002年 | 70篇 |
2001年 | 48篇 |
2000年 | 46篇 |
1999年 | 62篇 |
1998年 | 65篇 |
1997年 | 52篇 |
1996年 | 48篇 |
1995年 | 34篇 |
1994年 | 23篇 |
1993年 | 34篇 |
1992年 | 18篇 |
1991年 | 12篇 |
1990年 | 7篇 |
1989年 | 10篇 |
1988年 | 7篇 |
1987年 | 8篇 |
1986年 | 4篇 |
1985年 | 5篇 |
1984年 | 7篇 |
1983年 | 4篇 |
1982年 | 4篇 |
1981年 | 2篇 |
1979年 | 2篇 |
1975年 | 1篇 |
1974年 | 1篇 |
1958年 | 2篇 |
1957年 | 4篇 |
排序方式: 共有3771条查询结果,搜索用时 187 毫秒
31.
勉略构造带作为秦岭造山带内重要的构造边界,关于其构造属性及晚古生代以来的地质背景,一直是学术界争论的焦点。碎屑锆石U-Pb年代学在限定地层单元的最大沉积年龄、研究区域构造岩浆事件及约束构造地质背景等方面行之有效。基于此,通过对勉略带内五郎坪北侧两河口变沉积地层和侵入其中的变形花岗岩脉体进行LA-ICP-MS锆石U-Pb年代学研究。获得2件变形花岗岩脉的结晶年龄均为406±1Ma。碎屑锆石主年龄谱分别为422~456Ma和558~826Ma,峰值年龄为441Ma和771Ma、813Ma,次级年龄谱分别为942~1495Ma和1658~2981Ma,峰值年龄不明显。依据最小一组碎屑锆石的峰值年龄(441Ma),和侵入其中的变形花岗岩脉(406±0.6Ma),限定该变沉积地层形成时代为406~441Ma(S_1-D_1)。碎屑锆石年龄谱显示该套变沉积地层物质来源较为复杂,其中秦岭造山带及扬子板块北缘早古生代、新元古代岩浆岩为其提供了74%±的物源,古老变质基底为其提供了26%±的物源。通过与区域上已有资料对比,认为勉略构造带内晚古生代沉积地层形成环境与邻区大致相同,且本次所获得的变沉积岩碎屑锆石年龄谱也与邻区泥盆系相似。综合认为,勉略构造带与邻区在晚古生代应属同一构造环境,晚古生代"勉略海盆"应当包括整个南秦岭。 相似文献
32.
C. E. Runge A. Kubo B. Kiefer Y. Meng V. B. Prakapenka G. Shen R. J. Cava T. S. Duffy 《Physics and Chemistry of Minerals》2006,33(10):699-709
The equation of state of MgGeO3 perovskite was determined between 25 and 66 GPa using synchrotron X-ray diffraction with the laser-heated diamond anvil cell. The data were fit to a third-order Birch–Murnaghan equation of state and yielded a zero-pressure volume (V 0) of 182.2 ± 0.3 Å3 and bulk modulus (K 0) of 229 ± 3 GPa, with the pressure derivative (K′0 = (?K 0/?P) T ) fixed at 3.7. Differential stresses were evaluated using lattice strain theory and found to be typically less than about 1.5 GPa. Theoretical calculations were also carried out using density functional theory from 0 to 205 GPa. The equation of state parameters from theory (V 0 = 180.2 Å3, K 0 = 221.3 GPa, and K′0 = 3.90) are in agreement with experiment, although theoretically calculated volumes are systematically lower than experiment. The properties of the perovskite phase were compared to MgGeO3 post-perovskite phase near the observed phase transition pressure (~65 GPa). Across the transition, the density increased by 2.0(0.7)%. This is in excellent agreement with the theoretically determined density change of 1.9%; however both values are larger than those for the (Mg,Fe)SiO3 phase transition. The bulk sound velocity change across the transition is small and is likely to be negative [?0.5(1.6)% from experiment and ?1.2% from theory]. These results are similar to previous findings for the (Mg,Fe)SiO3 system. A linearized Birch–Murnaghan equation of state fit to each axis yielded zero-pressure compressibilities of 0.0022, 0.0009, and 0.0016 GPa?1 for the a, b, and c axis, respectively. Magnesium germanate appears to be a good analog system for studying the properties of the perovskite and post-perovskite phases in silicates. 相似文献
33.
The sedimentary environments are the intrinsic factor controlling the mechanical properties of clastic rocks. Examining the relationship between rock sedimentary environments and rock mechanical properties gives a better understanding of rock deformation and failure mechanisms. In this study, more than 55 samples in coal measures were taken from seven different lithologic formations in eastern China. Using the optical microscope the sedimentary characteristics, such as components of clastic rocks and sizes of clastic grains were quantitatively tested and analyzed. The corresponding mechanical parameters were tested using the servo-controlled testing system. Different lithologic attributes in the sedimentary rocks sampled different stress–strain behaviors and failure characteristics under different confining pressures, mainly due to different compositions and textures. Results demonstrate that clastic rocks have the linear best-fit for Mohr-Coulomb failure criterion. The elastic moduli in clastic rocks are highly dependent upon confining pressures, unlike hard rocks. The envelope lines of the mechanical properties versus the contents of quartz, detritus of the grain diameter of more than 0.03 mm, and grain size in clastic rocks are given. The compressive strength or elastic modulus and the grain diameter have a non-monotonic relation and demonstrate the “grain-diameter softening” effect. 相似文献
34.
各位来宾,各位代表,同志们:国土资源信息化建设成果展览,今天在美丽的昆明市隆重开幕了。我谨代表国土资源部,对展览的成功举办表示热烈的祝贺!向参与这次展览的各界代表和朋友们表示诚挚的问候!向各位来宾和同志们表示衷心的感谢! 相似文献
35.
本文介绍了大范围卫星影像彩色镶嵌图的制作流程.对于大范围卫星影像彩色镶嵌图制作的技术难点(去云、拼接、调色),文章进行了重点介绍并提出技术解决办法.利用MODIS卫星数据制作了两幅全国彩色影像镶嵌图:一幅为红波段(B1)、绿波段(B4)和蓝波段(B3)构成的真彩色合成影像:一幅为红波段(B1).近红外波段(B2)和蓝波段(B3)构成的假彩色合成影像.两幅影像色彩精美,信息量丰富. 相似文献
36.
37.
38.
39.
40.