全文获取类型
收费全文 | 276篇 |
免费 | 69篇 |
国内免费 | 45篇 |
专业分类
测绘学 | 65篇 |
大气科学 | 38篇 |
地球物理 | 31篇 |
地质学 | 126篇 |
海洋学 | 53篇 |
天文学 | 2篇 |
综合类 | 35篇 |
自然地理 | 40篇 |
出版年
2024年 | 1篇 |
2023年 | 14篇 |
2022年 | 17篇 |
2021年 | 13篇 |
2020年 | 19篇 |
2019年 | 22篇 |
2018年 | 13篇 |
2017年 | 20篇 |
2016年 | 20篇 |
2015年 | 23篇 |
2014年 | 14篇 |
2013年 | 20篇 |
2012年 | 15篇 |
2011年 | 17篇 |
2010年 | 18篇 |
2009年 | 8篇 |
2008年 | 10篇 |
2007年 | 10篇 |
2006年 | 8篇 |
2005年 | 6篇 |
2004年 | 7篇 |
2003年 | 3篇 |
2002年 | 7篇 |
2001年 | 3篇 |
2000年 | 5篇 |
1999年 | 8篇 |
1998年 | 5篇 |
1997年 | 9篇 |
1996年 | 4篇 |
1995年 | 5篇 |
1994年 | 11篇 |
1993年 | 12篇 |
1992年 | 6篇 |
1991年 | 7篇 |
1990年 | 2篇 |
1988年 | 1篇 |
1987年 | 1篇 |
1986年 | 3篇 |
1984年 | 2篇 |
1980年 | 1篇 |
排序方式: 共有390条查询结果,搜索用时 15 毫秒
21.
In this paper, four problems are discussed: (1) the monsoon circulation over southern Asia; (2) the seasonal variation of
the general circulation of the atmosphere; (3) the influence of the monsoon on the rainfall in southwestern China; and (4)
the source region of water vapor for the rainfall in the Changjiang valley. 相似文献
22.
23.
根据地质、地球化学和资源总量预测等方法的综合研究表明,在阿尔泰高山区红山咀断裂以北宽20~30km,东西长约150km地带为一重要金成矿带。金矿赋存于晚古生代陆相酸—中酸性火山岩地层中,空间上受冰长石-黄铁绢英岩化蚀变带严格控制,是以毒砂、辉锑矿等金属硫化物为主要载体的层控浅成低温热液溶滤型金矿,也是一种新的重要的金矿工业类型。 相似文献
24.
在矿图绘制过程中,AUTOCAD和数据库系统(DBMS)之间的来回切换而引发的种种问题一直难以解决。本文以ASE为基础,介绍一种新型的矿图属性数据数据管理方法,为CAD与DBMS的合理集成提供了一种新途径。 相似文献
25.
26.
28.
Yifeng Chen Shaohua Hu Chuangbing Zhou Lanru Jing 《Rock Mechanics and Rock Engineering》2014,47(5):1775-1791
This paper presents a study on the initiation and progress of anisotropic damage and its impact on the permeability variation of crystalline rocks of low porosity. This work was based on an existing micromechanical model considering the frictional sliding and dilatancy behaviors of microcracks and the recovery of degraded stiffness when the microcracks are closed. By virtue of an analytical ellipsoidal inclusion solution, lower bound estimates were formulated through a rigorous homogenization procedure for the damage-induced effective permeability of the microcracks-matrix system, and their predictive limitations were discussed with superconducting penny-shaped microcracks, in which the greatest lower bounds were obtained for each homogenization scheme. On this basis, an empirical upper bound estimation model was suggested to account for the influences of anisotropic damage growth, connectivity, frictional sliding, dilatancy, and normal stiffness recovery of closed microcracks, as well as tensile stress-induced microcrack opening on the permeability variation, with a small number of material parameters. The developed model was calibrated and validated by a series of existing laboratory triaxial compression tests with permeability measurements on crystalline rocks, and applied for characterizing the excavation-induced damage zone and permeability variation in the surrounding granitic rock of the TSX tunnel at the Atomic Energy of Canada Limited’s (AECL) Underground Research Laboratory (URL) in Canada, with an acceptable agreement between the predicted and measured data. 相似文献
29.
30.
Shaohua Zhou 《地学学报》1996,8(6):514-524
An analytical solution has been derived for the steady-state geotherm of the continental lithosphere, using an empirical thermal conductivity model that incorporates the experimentally observed temperature and pressure effect. Based on recent global compilations of crustal thickness and heat flow data, a standard continental lithosphere is re-defined by a global mean model with total crustal thickness of 40 km and surface heat flow of 55 mWm-2 (within which 28 mWm-2 is assumed to be derived from deep mantle source). The thickness of the continental lithosphere (≅125 km), consistent with previous models, is given by the depth at which the geotherm intersects the potential asthenosphere temperature of 1280°C. It is shown that the new steady-state geotherm is much hotter than that based on the previously adopted model where material thermal conductivity is assumed to be constant (≅3.14 W/m/k) throughout the lithosphere. The consequence of this re-evaluation of pre-extension thermal structure in the lithosphere is that the minimum stretching factor required to cause the onset of dry mantle partial melting can be 15–20% lower than the previous estimate. Also, if minor amounts of water or other volatile element or dry basalt are present in the upper mantle, melting of the subcontirfental mantle is very likely to occur for any geotherms constructed using surface heat flows > 30 mWm-2 . 相似文献