全文获取类型
收费全文 | 3769篇 |
免费 | 869篇 |
国内免费 | 1175篇 |
专业分类
测绘学 | 190篇 |
大气科学 | 1538篇 |
地球物理 | 976篇 |
地质学 | 1811篇 |
海洋学 | 752篇 |
天文学 | 64篇 |
综合类 | 234篇 |
自然地理 | 248篇 |
出版年
2024年 | 22篇 |
2023年 | 45篇 |
2022年 | 124篇 |
2021年 | 137篇 |
2020年 | 162篇 |
2019年 | 198篇 |
2018年 | 126篇 |
2017年 | 158篇 |
2016年 | 147篇 |
2015年 | 203篇 |
2014年 | 237篇 |
2013年 | 213篇 |
2012年 | 232篇 |
2011年 | 235篇 |
2010年 | 212篇 |
2009年 | 276篇 |
2008年 | 269篇 |
2007年 | 346篇 |
2006年 | 277篇 |
2005年 | 272篇 |
2004年 | 235篇 |
2003年 | 200篇 |
2002年 | 199篇 |
2001年 | 155篇 |
2000年 | 148篇 |
1999年 | 137篇 |
1998年 | 143篇 |
1997年 | 120篇 |
1996年 | 107篇 |
1995年 | 77篇 |
1994年 | 85篇 |
1993年 | 59篇 |
1992年 | 63篇 |
1991年 | 60篇 |
1990年 | 37篇 |
1989年 | 22篇 |
1988年 | 33篇 |
1987年 | 12篇 |
1986年 | 6篇 |
1985年 | 6篇 |
1984年 | 1篇 |
1983年 | 1篇 |
1982年 | 3篇 |
1981年 | 3篇 |
1980年 | 4篇 |
1979年 | 1篇 |
1978年 | 3篇 |
1976年 | 1篇 |
1971年 | 1篇 |
排序方式: 共有5813条查询结果,搜索用时 15 毫秒
101.
102.
103.
104.
中国大陆壳内与上地幔高导层成因及唐山地震机理研究 总被引:25,自引:2,他引:25
文中首先给出了中国大陆上地幔高导层埋深图 ,对其物理成因作了解释。然后给出了中国大陆壳内高导层分布埋深图 ,因人们对壳内高导层的成因有多种看法 ,所以文中进行了讨论 ,并认为卤水成因说更有说服力。文中对壳内与上地幔高导层构造成因作了简要阐述。最后 ,由于壳内和上地幔高导层分布埋深与强地震的分布有密切的关系 ,所以作为实例 ,文中给出了唐山地区地壳结构 ,阐述了地壳内深部流体在地震中的作用 ,并给出了主要证据。 相似文献
105.
Crustal structure beneath the Songpan—Garze orogenic belt 总被引:2,自引:0,他引:2
The Benzilan-Tangke deepseismic sounding profile in the western Sichuan region passes through the Song-pan-Garze orogenic belt with trend of NNE.Based on the travel times and the related amplitudes of phases in the record sections,the 2-D P-wave crustal structure was ascertained in this paper.The velocity structure has quite strong lateral variation along the profile.The crust is divided into 5layers,where the first,second and third layer belong to the upper crust,the forth and fifth layer belong to the lower crust.The low velocity anomaly zone gener-ally exists in the central part of the upper crust on the profile,and it integrates into the overlying low velocity basement in the area to the north of Ma‘erkang.The crustal structure in the section can be divided into 4parts:in the south of Garze-litang fault,between Garze-Litang fault and Xianshuihe fault,between Xianshuihe fault and Longriba fault and in the north of Longriba fault,which are basically coincided with the regional tectonics division.The crustal thickness decreases from southwest to northeast along the profile,that is ,from62km in the region of the Jinshajiang River to 52km in the region of the Yellow River.The Moho discontinuity does not obviously change across the Xianshuihe fault basesd on the PmP phase analysis.The crustal average velocity along the profile is lower,about 6.30 km/s.The Benzilan-Tangke profile reveals that the crust in the study area is orogenic.The Xianshuihe fault belt is located in the central part of the profile,and the velocity is positive anomaly on the upper crust,and negative anomaly on the lower crust and upper mantle.It is considered as a deep tectonhic setting in favor of strong earthquake‘s accumulation and occurrence. 相似文献
106.
107.
指出了共线条件方程式教学中应注意的一些问题:共线条件方程式是联立的两个平面方程式,存在双主距(fx,fy)时的几何概念,以及它的变换式与直接线性变换关系式的异同点。 相似文献
108.
The characteristic features of the marine boundary layer (MBL) over the Bay of Bengal during the southwest monsoon and the
factors influencing it are investigated. The Bay of Bengal and Monsoon Experiment (BOBMEX) carried out during July–August
1999 is the first observational experiment under the Indian Climate Research Programme (ICRP). A very high-resolution data
in the vertical was obtained during this experiment, which was used to study the MBL characteristics off the east coast of
India in the north and south Bay of Bengal. Spells of active and suppressed convection over the Bay were observed, of which,
three representative convective episodes were considered for the study. For this purpose a one-dimensional multi-level PBL
model with a TKE-ε closure scheme was used. The soundings, viz., the vertical profiles of temperature, humidity, zonal and
meridional component of wind, obtained onboard ORV Sagar Kanya and from coastal stations along the east coast are used for
the study. The temporal evolution of turbulent kinetic energy, marine boundary layer height (MBLH), sensible and latent heat
fluxes and drag coefficient of momentum are simulated for different epochs of monsoon and monsoon depressions during BOBMEX-99.The
model also generates the vertical profiles of potential temperature, specific humidity, zonal and meridional wind. These simulated
values compared reasonably well with the observations available from BOBMEX. 相似文献
109.
110.
根据南海季风试验(SCSMEX)期间南海内区的三个ATLAS(Autonomous Temperature Line Acquisition System)锚碇浮标资料(1998年4月~1999年4月),采用谐波分析方法对南海上层海洋水温年循环、半年循环加以分离,发现无论在年循环还是在半年循环尺度上,18°N附近SCS1站与13°N附近SCS3站的水温变化次表层与表层呈反位相;15°20′N附近SCS2站水温变化基本上次表层与表层同位相.这说明不同区域上层海洋热变化受不同的正压与斜压模态控制.其次,SCS2、SCS3两点水温年循环振幅均在次表层达到极值;而SCS1在表层达到极大值,在100 m深度达到次极大值.3个站位水温半年循环振幅极值均出现在次表层内,这说明该层内的水温半年循环在温度变化趋势中所占的权重比在表层的权重大. 相似文献