全文获取类型
收费全文 | 4458篇 |
免费 | 1055篇 |
国内免费 | 1410篇 |
专业分类
测绘学 | 717篇 |
大气科学 | 565篇 |
地球物理 | 827篇 |
地质学 | 2902篇 |
海洋学 | 801篇 |
天文学 | 87篇 |
综合类 | 309篇 |
自然地理 | 715篇 |
出版年
2024年 | 33篇 |
2023年 | 75篇 |
2022年 | 266篇 |
2021年 | 305篇 |
2020年 | 260篇 |
2019年 | 313篇 |
2018年 | 269篇 |
2017年 | 266篇 |
2016年 | 265篇 |
2015年 | 267篇 |
2014年 | 290篇 |
2013年 | 355篇 |
2012年 | 398篇 |
2011年 | 389篇 |
2010年 | 379篇 |
2009年 | 371篇 |
2008年 | 371篇 |
2007年 | 332篇 |
2006年 | 329篇 |
2005年 | 307篇 |
2004年 | 221篇 |
2003年 | 167篇 |
2002年 | 185篇 |
2001年 | 163篇 |
2000年 | 124篇 |
1999年 | 57篇 |
1998年 | 25篇 |
1997年 | 20篇 |
1996年 | 19篇 |
1995年 | 8篇 |
1994年 | 8篇 |
1993年 | 6篇 |
1992年 | 8篇 |
1991年 | 5篇 |
1990年 | 11篇 |
1989年 | 7篇 |
1988年 | 2篇 |
1987年 | 6篇 |
1986年 | 2篇 |
1985年 | 5篇 |
1984年 | 5篇 |
1982年 | 3篇 |
1981年 | 2篇 |
1979年 | 2篇 |
1976年 | 5篇 |
1975年 | 3篇 |
1974年 | 4篇 |
1958年 | 1篇 |
1957年 | 3篇 |
1954年 | 2篇 |
排序方式: 共有6923条查询结果,搜索用时 46 毫秒
991.
Landslides triggered by slipping-fault-generated earthquake on a plateau: an example of the 14 April 2010, Ms 7.1, Yushu, China earthquake 总被引:3,自引:1,他引:2
On 14 April 2010 at 07:49 (Beijing time), a catastrophic earthquake with Ms 7.1 struck Yushu County, Qinghai Province, China. A total of 2,036 landslides were interpreted from aerial photographs and satellite images, verified by selected field checking. These landslides cover about a total area of 1.194 km2. The characteristics and failure mechanisms of these landslides are presented in this paper. The spatial distribution of the landslides is evidently strongly controlled by the locations of the main co-seismic surface fault ruptures. The landslides commonly occurred close together. Most of the landslides are small; there were only 275 individual landslide (13.5 % of the total number) surface areas larger than 1,000 m2. The landslides are of various types. They are mainly shallow, disrupted landslides, but also include rock falls, deep-seated landslides, liquefaction-induced landslides, and compound landslides. Four types of factors are identified as contributing to failure along with the strong ground shaking: natural excavation of the toes of slopes, which mean erosion of the base of the slope, surface water infiltration into slopes, co-seismic fault slipping at landslide sites, and delayed occurrence of landslides due to snow melt or rainfall infiltration at sites where slopes were weakened by the co-seismic ground shaking. To analyze the spatial distribution of the landslides, the landslide area percentage (LAP) and landslide number density (LND) were compared with peak ground acceleration (PGA), distance from co-seismic main surface fault ruptures, elevation, slope gradient, slope aspect, and lithology. The results show landslide occurrence is strongly controlled by proximity to the main surface fault ruptures, with most landslides occurring within 2.5 km of such ruptures. There is no evident correlation between landslide occurrences and PGA. Both LAP and LND have strongly positive correlations with slope gradient, and additionally, sites at elevations between 3,800 and 4,000 m are relatively susceptible to landslide occurrence; as are slopes with northeast, east, and southeast slope aspects. Q4 al-pl, N, and T3 kn 1 have more concentrated landslide activity than others. This paper provides a detailed inventory map of landslides triggered by the 2010 Yushu earthquake for future seismic landslide hazard analysis and also provides a study case of characteristics, failure mechanisms, and spatial distribution of landslides triggered by slipping-fault generated earthquake on a plateau. 相似文献
992.
993.
H. Md. Azamathulla Yong Chong Cuan Aminuddin Ab. Ghani Chun Kiat Chang 《Arabian Journal of Geosciences》2013,6(9):3469-3480
This study presents gene expression programming (GEP), an extension of genetic programming, as an alternative approach to modeling the suspended sediment load relationship for the three Malaysian rivers. In this study, adaptive neuro-fuzzy inference system (ANFIS), regression model, and GEP approaches were developed to predict suspended load in three Malaysian rivers: Muda River, Langat River, and Kurau River [ANFIS (R 2?=?0.93, root mean square error (RMSE)?=?3.19, and average error (AE)?=?1.12) and regression model (R 2?=?0.63, RMSE?=?13.96, and AE?=?12.69)]. Additionally, the explicit formulations of the developed GEP models are presented (R 2?=?0.88, RMSE?=?5.19, and AE?=?6.5). The performance of the GEP model was found to be acceptable compare to ANFIS and better than the conventional models. 相似文献
994.
995.
提要:铜绿山岩体的主要岩石类型为石英正长闪长玢岩,其次是闪长岩、石英闪长岩和闪长玢岩。利用LA-ICPMS和LA-MC-ICPMS对岩石中的锆石进行微区原位U-Pb年龄和Lu-Hf同位素测定,结果表明,该岩体至少有三次以上的侵入活动,分别为150 Ma、145 Ma和140 Ma,从西到东、由深到浅侧向迁移侵位,分别形成鸡冠嘴矿区深部的石英闪长岩和Ⅶ号铜金矿体,鸡冠嘴矿区较浅部的闪长岩和Ⅰ、Ⅱ、Ⅲ号等铜金矿体,铜绿山矿区及其周边的石英正长闪长玢岩和铜绿山、鲤泥湖、桃花嘴等铁铜矿床。岩浆锆石和继承锆石的U-Pb年龄和Hf同位素等信息显示,岩体的源区物质为混含有少量亏损地幔成分的古元古代(约1730 Ma)下地壳物质,并有中元古代晚期(1100~1200 Ma)和新元古代(800 Ma)地壳物质的加入。不同类型岩石的物源组成有明显差别,并形成不同的矿床。石英闪长岩和闪长岩形成铜金矿床,可能与其岩浆源区物质含有地幔成分有关。在继承锆石中获得新太古代、中太古代、古元古代、中元古代晚期和新元古代五组年龄数据,与宜昌崆岭群TTG片麻岩,京山、宁乡、镇远煌斑岩筒,宜昌莲沱砂岩、石门渫水河组(莲沱组)凝灰岩中的锆石年龄可以对比,表明鄂东南地区与扬子陆块其他地区的地壳演化历史基本一致,深部同样存在古元古代和太古宙基底。 相似文献
996.
提要:云南卓玛铅锌矿位于义敦岛弧南端的中甸弧,矿体产于印支期石英二长斑岩中,受断裂破碎带控制。通过对非矿斑岩、碎裂斑岩矿石、脉状矿石的稀土元素及矿石方铅矿硫、铅同位素的研究,表明非矿斑岩与矿石的稀土元素地球化学特征相似,矿石与斑岩同源。方铅矿的δ34S变化范围为-0.01‰~-2.90‰,为幔源岩浆硫,铅同位素206Pb/204Pb为18.0959~18.1119,207Pb/204Pb为15.6118~15.6191,208Pb/204Pb为38.2515~38.2918,矿石铅主要来自造山环境,源区属于以幔源铅为主的壳幔混合源。矿区铅锌矿化富集与印支晚期卓玛复式斑岩体密切相关,矿床属受断裂破碎带控制的岩浆热液充填-交代型矿床。 相似文献
997.
998.
999.
南海热带对流季节内振荡对江淮流域旱涝影响的初步分析 总被引:9,自引:6,他引:9
使用TBB17年逐月、候平均资料和欧亚500hPa候平均高度距平场,计算了南海地区逐月TBB的标准差,分析其时空分布特征。采用带通滤波方法,分析了江淮流域旱(1985年)、涝(1991、1998年)年南海地区TBB季节内振荡及其经向传播特征。结果表明,江淮流域涝年,南海地区TBB30~60d和10~20d振荡十分活跃,向北传播非常明显。当TBB强对流位相传播到30°N附近的副热带地区时,激发其对流扰动加强,造成江淮流域集中暴雨。而旱年则相反。南海和30°N地区对流活动的强弱差异与500hPa候平均高度距平场的遥相关揭示出江淮流域旱涝年波列结构有很大的不同。 相似文献
1000.