全文获取类型
收费全文 | 454篇 |
免费 | 139篇 |
国内免费 | 127篇 |
专业分类
测绘学 | 66篇 |
大气科学 | 174篇 |
地球物理 | 124篇 |
地质学 | 174篇 |
海洋学 | 26篇 |
天文学 | 48篇 |
综合类 | 39篇 |
自然地理 | 69篇 |
出版年
2023年 | 5篇 |
2022年 | 17篇 |
2021年 | 20篇 |
2020年 | 18篇 |
2019年 | 16篇 |
2018年 | 18篇 |
2017年 | 29篇 |
2016年 | 34篇 |
2015年 | 30篇 |
2014年 | 20篇 |
2013年 | 38篇 |
2012年 | 32篇 |
2011年 | 24篇 |
2010年 | 28篇 |
2009年 | 28篇 |
2008年 | 23篇 |
2007年 | 28篇 |
2006年 | 28篇 |
2005年 | 31篇 |
2004年 | 25篇 |
2003年 | 16篇 |
2002年 | 29篇 |
2001年 | 11篇 |
2000年 | 20篇 |
1999年 | 21篇 |
1998年 | 16篇 |
1997年 | 21篇 |
1996年 | 17篇 |
1995年 | 16篇 |
1994年 | 11篇 |
1993年 | 10篇 |
1992年 | 7篇 |
1991年 | 8篇 |
1990年 | 5篇 |
1989年 | 5篇 |
1988年 | 6篇 |
1987年 | 1篇 |
1986年 | 1篇 |
1985年 | 2篇 |
1984年 | 1篇 |
1983年 | 3篇 |
1980年 | 1篇 |
排序方式: 共有720条查询结果,搜索用时 15 毫秒
91.
92.
93.
福建省古生代至中生代大地构造演化的格架 总被引:10,自引:0,他引:10
松溪—长汀断裂带和福州—永定断裂带是控制福建古生代及以后大地构造演化的两条北东东向的断裂带。地质地球化学资料表明,前者是加里东期的地体碰撞带,沿线分布了构造混杂岩、变质超基性岩体、具有角闪岩相和中压矿物的变质岩以及同碰撞型花岗岩体,以后又发育为A型俯冲带;后者是发育于加里东构造层之上的海西期张裂带,在形成海西期的福州—永定海峡的同时,产生了石炭纪海底双模式火山岩及层控铁矿,印支期的碰撞活动使海峡封闭并发育A型俯冲作用。由此,北东东向的松溪—长汀断裂带和福州—永定断裂带可以将福建划分为三个古生代的构造地层地体:闽北地体、闽中地体和闽东南地体。通过对福建省古生代地体构造分析、古地磁测量及古地理重建,展现在我们眼前是:华南(其中包括福建)在古生代中期从冈瓦纳大陆分离出来后,横渡特提斯海,在古生代末至中生代初到达劳亚大陆,与中朝板块碰撞引起了福建地体间强烈的造山运动。 相似文献
94.
The wavelets and hierarchies of the climate system 总被引:1,自引:0,他引:1
Summary Wavelet analysis of global mean temperature data, the drought-flood data of the past 500 years in China, and the temperature time series of Shanghai, highlights the following: (1) the climatic wavelets depend on the hierarchies of a climate system; (2) for different time scales or hierarchies, a climate system may have different catastrophic points and periods; (3) for different time scales or hierarchies, variation of the Southern Hemisphere temperature has an obvious phase-lag compared with that of the Northern Hemisphere and the catastrophe points also lag behind; (4) in a cold-warm period, the cold semi-period of the Northern Hemisphere is obviously longer than the warm one; (5) for different hierarchies or time scales, there exists a phase-lag for the droughtflood variation in China moving gradually with latitude from north to south. Finally, a new technique of climate diagnosis, the phase curve of wavelets, is put forward in this paper.With 6 FiguresSupported by Chinese NKPFR. 相似文献
95.
96.
97.
98.
The interaction of turbulent and radiative transfer applied to a number of plausible atmospheric situations in the surface layer under the stably stratified condition is discussed.The calculated results show that the long-wave radiative flux has a great influence upon the thermal structure of the surface layer, and that it usually acts in such a way as to weaken the thickness of the constant turbulent heat flux layer. In the case of low wind velocities and strongly stable stratifications, the thickness of the turbulent heat flux layer will become very thin and/or inexistent. 相似文献
99.
Deep-large faults in the central continental margin of eastern China are well developed. Based on the regularity of spatial
and temporal distribution of the faults, four fault systems were divided: the Yanshan orogenic belt fault system, the Qinling-Dabie-Sulu
orogenic belt fault system, the Tanlu fault system and the East China Sea shelf basin-Okinawa trough fault system. The four
fault systems exhibit different migration behaviors. The Yanshan orogenic belt fault system deflected from an EW to a NE direction,
then to a NNE direction during the Indo-Chinese epoch-Yanshanian epoch. The thrust-nappe strength of the Qinling-Dabie orogenic
belt fault system showed the tendency that the strength was greater in the south and east, but weaker in the north and west.
This fault system faulted in the east and folded in the west from the Indo-Chinese epoch to the early Yanshanian epoch. At
the same time, the faults also had a diachronous migration from east to west from the Indo-Chinese epoch to the early Yanshanian
epoch. On the contrary, the thrust-nappe strength was greater in the north and west, weaker in the south and east during the
late Yanshanian epoch-early Himalayan epoch. The Tanlu fault system caused the basin to migrate from west to east and south
to north. The migration regularity of the East China Sea shelf basin-Okinawa trough fault system shows that the formation
age became younger in the west. The four fault systems and their migration regularities were respectively the results of four
different geodynamic backgrounds. The Yanshan orogenic belt fault system derived from the intracontinental orogeny. The Qinling-Dabie-Sulu
orogenic belt fault system derived from the collision of plates and intracontinental subduction. The Tanlu fault system derived
from the strike-slip movement and the East China Sea shelf basin-Okinawa trough fault system derived from plate subduction
and retreat of the subduction belt.
Translated from Journal of Jilin University (Earth Science Edition), 2005, 35(5): 554–563 [译自: 吉林大学学报 (地球科学版)] 相似文献
100.
阐述了移动GIS的概念,提出了一个由表示层、逻辑层和数据层所构成的分布式体系结构,介绍了移动接入技术、移动访问技术、移动定位技术、嵌入式技术和语音技术等关键技术。 相似文献