全文获取类型
收费全文 | 2136篇 |
免费 | 446篇 |
国内免费 | 738篇 |
专业分类
测绘学 | 125篇 |
大气科学 | 661篇 |
地球物理 | 487篇 |
地质学 | 1135篇 |
海洋学 | 315篇 |
天文学 | 47篇 |
综合类 | 218篇 |
自然地理 | 332篇 |
出版年
2024年 | 18篇 |
2023年 | 52篇 |
2022年 | 119篇 |
2021年 | 148篇 |
2020年 | 111篇 |
2019年 | 153篇 |
2018年 | 131篇 |
2017年 | 135篇 |
2016年 | 146篇 |
2015年 | 120篇 |
2014年 | 144篇 |
2013年 | 114篇 |
2012年 | 112篇 |
2011年 | 109篇 |
2010年 | 106篇 |
2009年 | 110篇 |
2008年 | 100篇 |
2007年 | 85篇 |
2006年 | 48篇 |
2005年 | 61篇 |
2004年 | 60篇 |
2003年 | 77篇 |
2002年 | 62篇 |
2001年 | 66篇 |
2000年 | 77篇 |
1999年 | 123篇 |
1998年 | 113篇 |
1997年 | 95篇 |
1996年 | 80篇 |
1995年 | 85篇 |
1994年 | 74篇 |
1993年 | 60篇 |
1992年 | 52篇 |
1991年 | 38篇 |
1990年 | 34篇 |
1989年 | 22篇 |
1988年 | 11篇 |
1987年 | 12篇 |
1986年 | 16篇 |
1985年 | 8篇 |
1984年 | 3篇 |
1983年 | 7篇 |
1982年 | 7篇 |
1981年 | 4篇 |
1980年 | 4篇 |
1979年 | 1篇 |
1978年 | 5篇 |
1977年 | 1篇 |
1976年 | 1篇 |
排序方式: 共有3320条查询结果,搜索用时 15 毫秒
231.
Wang Siyuan Xiao Qibing Zeng Jianguo Faculty of Earth Resources China University of Geosciences Wuhan 《中国地质大学学报(英文版)》2001,12(1)
-,The well-known Suichang silvengold field is located inZhejiang Province of SOutheast China. It is the largest silver-gold deposit associated with copper and zinc in the Cathaysianmetallogenic province.There are a series of silver-gold dePOsits in the shear zonesof Proterozoic gneiss terrene, Suichang region. The volcanicapparatus at Mesozoic has complicated rpineralization. Respectively, there are two pieces of understanding on the origin ofore-formigg nuid: (l ) metamorphic fluid (Lia… 相似文献
232.
在分析合成孔径雷达(SAR)成象机理及雪盖参数散射特性的基础上,利用航天飞机承载的成象雷达(SIR—C)获取的多波段、多极化SAR数据,进行提取雪盖信息的实验。结果表明C波段HH、VV影象能很好地区别湿雪与非雪盖区,而区分干雪与岩石较困难;L波段HH、VV影象较容易将雪盖同其它物体区分开;C、L波段的交叉极化HV、VH区分干雪与岩石效果很好。故利用多波段、多极化SAR进行雪盖制图是可行的。 相似文献
233.
A total of 11 earthquakes with 15 Rayleigh wave paths, recorded at 11 broadband digital PASSCAL seismometers installed in
the Tibet Plateau by the Sino-U.S. joint research group, were used to determine the phase velocity and attenuation coefficient
of surface waves in periods of 10–130 s. The average shear wave velocity and quality factor {ie271-1} structures in the crust
and upper mantle were obtained in this region. The result shows the average {ie271-2} is low and there exists a high attenuation
({ie271-3}=93–141) layer in the crust. The depth range of the low {ie271-4} value layer (16–42 km) is consistent with the
range of low velocity layer (21–51 km) in the crust. Below 63 km in the lower crust, {ie271-5} decreases with depth from 114
to 34 at depth of 180 km. The low shear wave velocity and low value of {ie271-6} at the same depth range in the crust indicate
that the rocks in the range is probably melted or partially melted. According to the shear wave velocity structure, the average
thickness of the crust is about 71 km and a clear velocity discontiniuty appears at the depth of 51 km. The low-velocity zone
(4. 26 km/s) at depth of 96–180 km may be corresponding to the asthenosphere.
Contribution No. 96A0047, Institute of Geophysics, SSB, China.
This study was supported by the National Natural Science Foundation of China. 相似文献
234.
X. Zeng 《Meteorology and Atmospheric Physics》1996,60(4):207-224
Summary As an approach to study the mesoscale processes within a typhoon, an axisymmetric nonhydrostatic numerical model is developed without the use of convective parameterization. Many simulated characteristics are consistent with radar and aircraft observations, such as the maximum of vertical and tangential wind, the inflow concentrated near the surface, the outward slope of the eyewall updraft, etc. The model duplicates not only the outward propagation of mesoscale convective systems, but also the inward movement of convective rings, the rate of which coincides with the observation. Besides, the model gives good simulations of the life cycle of convective rings, and indicates that the convective rings far from the eyewall play important roles in the fluctuation of typhoon intensity. Numerical results also exhibit the existence of coupling between outer and inner core structure.Analyses of the simulations show that convective momentum transport generates local maximum absolute angular momentum in the middle and upper troposphere. The momentum anomaly results in symmetric instability, which provides the environment to form convective rings. While the momentum anomaly moves outward with the outflow in the middle and upper troposphere, it initiates a series of convective rings with aid of other direct factors, which explains the outward propagation of convective systems.The simulations exhibit the life cycle of a typical convective ring in terms of three stages, or the developing, mature and dissipating stage. Analysis shows that the symmetric instability and the convective instability promote each other, and their cooperation makes the life of convective rings longer.With 8 Figures 相似文献
235.
A total of 11 earthquakes with 15 Rayleigh wave paths, recorded at 11 broadband digital PASSCAL seismometers installed in the Tibet Plateau by the Sino-U.S. joint research group, were used to determine the phase velocity and attenuation coefficient of surface waves in periods of 10–130 s. The average shear wave velocity and quality factor {ie271-1} structures in the crust and upper mantle were obtained in this region. The result shows the average {ie271-2} is low and there exists a high attenuation ({ie271-3}=93–141) layer in the crust. The depth range of the low {ie271-4} value layer (16–42 km) is consistent with the range of low velocity layer (21–51 km) in the crust. Below 63 km in the lower crust, {ie271-5} decreases with depth from 114 to 34 at depth of 180 km. The low shear wave velocity and low value of {ie271-6} at the same depth range in the crust indicate that the rocks in the range is probably melted or partially melted. According to the shear wave velocity structure, the average thickness of the crust is about 71 km and a clear velocity discontiniuty appears at the depth of 51 km. The low-velocity zone (4. 26 km/s) at depth of 96–180 km may be corresponding to the asthenosphere. 相似文献
236.
A deterministic near-surface correction procedure is developed for multicomponent VSP data, shot using directional sources and recorded using three-component receivers. The method is capable of removing unwanted effects of acquisition such as unequal source strengths or misorientations, but may also remove near-surface multiples and anisotropy. This is of considerable benefit for obtaining accurate and consistent estimates of subsurface anisotropy from different source combinations. Application of the technique is illustrated using a dataset from the Romashkino reservoir in Russia, where three or four different directional sources are used at the same source locations. The technique corrects for the large discrepancies which exist between the estimates obtained using different source combinations. Application of the technique to three wells in the survey region reveals a nearly isotropic subsurface, except for a few isolated zones of moderate to high (2 to 8%) anisotropy which lie close to the expected depth for the reservoir. Although there is no significant correlation with the production figures for each well, the qS1 polarization azimuth within the reservoir does vary at each well location, suggesting that this may be a more sensitive indicator of reservoir Drocess. 相似文献
237.
不同成因类型煤中烷基环己烷和烷基苯的特征探讨 总被引:2,自引:0,他引:2
通过对藻煤、烛煤、腐殖煤共生煤层的分析,将不同成因类型煤中的烷基环己烷和烷基苯进行了比较。结果表明,不同成因类型煤中所含的烷基环己烷和烷基苯明显不同。各种成因类型煤中烷基环己烷和烷基苯所提供的母质信息与煤岩结果吻合。氧化环境不利于烷基环己烷和烷基苯的形成。烷基环己烷和烷基苯有时可以作为沉积环境和成熟度的标志。 相似文献
238.
论大气环流的季节划分和季节突变 Ⅰ:概念和方法 总被引:13,自引:4,他引:13
本工作系列讨论大气环流的季节划分和季节突变问题.本文是第一篇,提出普适的概念、理论和方法,使大气环流和其他气候场的季节划分和季节突变定义建立在客观定量的基础之上.首先用两个场的相关系数R作为其相似性度量,也可以用归范化的两个场之差的根方值d作为差异性的度量.当存在着冬、夏季的典型场F_n和F_s时,取任何时刻t函数F与F~*≡(F_w+F_s)/2之差F~'作为变量场,则其与F~'_w≡F_w-F~*的相关系数R_w(t)及标准根方差d_w(t)可以作为F与其冬季典型的相似性或差异性度量.R_w与d_w~2之间有一定关系,一般只研究R_w即可.(1)可以定义冬季对应于1≥R_w(t)>0.5,夏季为-1≤R_w(t)<-0.5,过渡季节为-0.5相似文献
239.
本文对开展地震宣传的形式分类及适度开展,如何建立与健全地震宣传网络,筹措地震宜传经费,完善地震宣传激励机制等进行了论述与探讨,分析了我国目前地震宣传工作存在的主要问题,并提出改进性意见。 相似文献
240.