全文获取类型
收费全文 | 1360篇 |
免费 | 307篇 |
国内免费 | 372篇 |
专业分类
测绘学 | 96篇 |
大气科学 | 385篇 |
地球物理 | 465篇 |
地质学 | 613篇 |
海洋学 | 167篇 |
天文学 | 46篇 |
综合类 | 111篇 |
自然地理 | 156篇 |
出版年
2024年 | 11篇 |
2023年 | 31篇 |
2022年 | 52篇 |
2021年 | 79篇 |
2020年 | 67篇 |
2019年 | 62篇 |
2018年 | 87篇 |
2017年 | 79篇 |
2016年 | 65篇 |
2015年 | 88篇 |
2014年 | 90篇 |
2013年 | 96篇 |
2012年 | 81篇 |
2011年 | 96篇 |
2010年 | 75篇 |
2009年 | 74篇 |
2008年 | 84篇 |
2007年 | 64篇 |
2006年 | 49篇 |
2005年 | 46篇 |
2004年 | 49篇 |
2003年 | 53篇 |
2002年 | 65篇 |
2001年 | 64篇 |
2000年 | 51篇 |
1999年 | 55篇 |
1998年 | 43篇 |
1997年 | 33篇 |
1996年 | 37篇 |
1995年 | 16篇 |
1994年 | 40篇 |
1993年 | 34篇 |
1992年 | 24篇 |
1991年 | 16篇 |
1990年 | 14篇 |
1989年 | 14篇 |
1988年 | 9篇 |
1987年 | 10篇 |
1986年 | 4篇 |
1985年 | 5篇 |
1984年 | 7篇 |
1983年 | 2篇 |
1982年 | 8篇 |
1981年 | 1篇 |
1980年 | 4篇 |
1977年 | 1篇 |
1974年 | 1篇 |
1964年 | 1篇 |
1958年 | 1篇 |
1949年 | 1篇 |
排序方式: 共有2039条查询结果,搜索用时 15 毫秒
861.
The early Cretaceous structure of NE China was a result of slab‐rollback‐driven extensional tectonics, characteristic of Western Pacific‐type continental margins. Oblique docking of a microcontinent along the Asian active margin in the early Late Cretaceous induced a compressional stress regime that brought about an Andean‐type continental margin development. Partitioning of contractional–transpressional strain across NE China produced a retroarc foreland basin system, comprising, from east to west, an orogenic wedge, a foredeep (Songliao basin), a forebulge (Great Xing'an Range) and a back‐bulge depozone (Hailar and Erlian basins). A sub‐circular lacustrine depozone in the pre‐existing Songliao basin evolved into a NNE‐trending depocentre near the forebulge and acquired a westward flowing fluvial–deltaic drainage system during the Campanian. Development of this retroarc foreland basin system signals a significant tectonic switch from a Western Pacific‐type to an Andean‐type continental margin evolution in the geological history of East Asia. 相似文献
862.
以湖南张家界田坪和大坪震旦系剖面为主要研究对象,开展了湘西北地区斜坡相区震旦系层序地层的划分和对比研究。根据斜坡相区三级层序的发育特点,将陡山沱组划分为5个三级层序(ZSQ1~5),灯影组划分为4个三级层序(ZSQ6~9)。其中,陡山沱组下部的4个三级层序(ZSQ1~4)构成震旦系下部的二级层序,陡山沱组顶部的三级层序ZSQ5和灯影组的4个三级层序(ZSQ6~9)构成震旦系上部的二级层序。斜坡相区与台地相区震旦系层序地层的划分基本一致,可实现相互对比;斜坡相区与盆地相区震旦系只能实现二级层序的对比。 相似文献
863.
864.
865.
866.
作为重要的海洋中尺度现象之一,中尺度涡的研究受到人们的关注和重视。随着数值模式的进一步发展、卫星资料的累积、时间更长以及更多更有效的海上实测数据的取得,使得综合利用实测资料、卫星遥感资料、再分析/数值预报产品等数据源,对中尺度涡进行自动识别与三维结构分析成为中尺度涡研究的主要方向之一。在前期对卫星遥感资料中尺度涡自动检测算法进行研究的基础上,开展多源资料中尺度涡三维结构分析方法研究,以表面漂流浮标运动轨迹为中尺度涡的判定依据,综合利用高度计观测、红外遥感观测、以及再分析/数值预报产品分析中尺度涡三维结构信息,在此基础上,提出中尺度涡研究的发展方向,为全面分析中尺度涡的时空特性提供技术途径,为中尺度涡的动力机制研究奠定基础。 相似文献
867.
Basal melting is an important factor affecting the stability of the ice shelf. The basal channel is formed from uneven melting, which also has an important impact on the stability of the ice shelf. Therefore, it has important scientific value to study the basal channel changes. This study combined datasets of Mosaics of Antarctica, Reference Elevation Model of Antarctica (REMA) and Operation IceBridge to study the temporal and spatial changes of basal channels at the Getz Ice Shelf in Antarctica. The relationships between the cross-sectional area and width of basal channel and those of its corresponding surface depression were statistically analyzed. Then, the changes of the basal channels of Getz Ice Shelf were derived from the ICESat observations and REMA digital elevation models (DEMs). After a detailed analysis of the factors affecting the basal channel changes, we found that the basal channels of Getz Ice Shelf were mainly concentrated in the eastern of the ice shelf, and most of them belonged to the ocean-sourced basal channel. From 2009 to 2016, the total length of the basal channel has increased by approximately 60 km. Affected by the warm Circumpolar Deep Water (CDW), significant changes in the basal channel occurred in the middle reaches of the Getz Ice Shelf. The change of the basal channels at the edge of the Getz Ice Shelf is significantly weaker than that in its middle and upper reaches. Especially in 2005–2012, the eastward wind on the ocean wind field and the westward wind around the continental shelf caused the invasion and upwelling of CDW. Meanwhile, the continuous warming of deep seawater also caused the deepening of the basal channel. During from 2012 to 2020, the fluctuations of the basal channels seem to be caused by the changes in temperature of CDW. 相似文献
868.
Transfer and transport of phosphorus and silica in the turbidity maximum zone of the Changjiang estuary 总被引:1,自引:0,他引:1
The concentration of suspended particulate matter (SPM), sedimentation flux, and various forms of phosphorus and silica in turbidity maximum zone (TMZ) in the Changjiang (Yangtze) estuary was studied. Based on the budget of P and Si, their mass balances in the TMZ were calculated. Results show that the variation in concentration of dissolved inorganic silicon (DISi) was mainly controlled by seawater dilution, while that of dissolved inorganic phosphorus (DIP) was considerably affected by the buffering of suspended matter and sediment. Our experiments showed that the sedimentation fluxes of SPM and particulate inorganic phosphorus (PIP), total particulate phosphorus (TPP), particulate inorganic silicon (PISi), and biological silicon (BSi) in the TMZ were 238.4 g m−2 d−1 and 28.3, 43.1, 79.0, 63.0 mg m−2 d−1, respectively. In addition, a simple method to estimate the ratio of resuspension of sediment in the TMZ was established, with which the rate in surface and bottom waters of the TMZ accounted for 55.7 and 66.1% of the total SPM, respectively, indicating that the sediment resuspension in the TMZ influenced significantly the mass balances of P and Si. Particulate adsorbed P (60.8%) and 35.5% of total particulate P discharged from the river were filtered and then deposited in the TMZ. The input flux of PIP from the river mouth was 55.9% of that of DIP, being important as biologically available P, while that of PISi was only 3.5% of DISi, showing that particulate adsorbed Si was much less important than particulate adsorbed P. 相似文献
869.
870.
Dust variation recorded by lacustrine sediments from arid Central Asia since ~ 15 cal ka BP and its implication for atmospheric circulation 总被引:1,自引:0,他引:1
Cheng-Bang An Jiaju Zhao Shichen Tao Yanbin Lv Weimiao Dong Hu Li Ming Jin Zongli Wang 《Quaternary Research》2011,75(3):566-573
A long dust history established using geological archives from dust provenance areas is necessary to understand the role of atmospheric dust in the global climate system better. Core sediments from a closed-basin groundwater-recharged lake in arid Central Asia were investigated using a multi-proxy approach (e.g. 14C AMS dating, pollen, and grain size) to trace the dust history since ~ 15 cal ka BP. Pollen analysis showed that before 7.9 cal ka BP, the vegetation was of desert type. After 7.9 cal ka BP, vegetation density increased, probably due to slightly increased moisture. The Chenopodiaceae-dominated desert expanded rapidly at 4.2–3.8 cal ka BP. Grain-size analysis was conducted for samples of lake deposits, modern aeolian dust, and dust trapped in snow, and the data showed that there was strong aeolian dust deposition at 11.8–11.1, 10.6–8, 6.1–4.9, and after 3.3 cal ka BP. This timing corresponds well with periods of increased terrestrial dust fluxes recorded by Greenland ice cores. Our study may document changes in the location and intensity of the Siberia High. These changes may play a more important role in the history of dust emission in arid Central Asia than previously thought. 相似文献