全文获取类型
收费全文 | 10291篇 |
免费 | 1804篇 |
国内免费 | 2359篇 |
专业分类
测绘学 | 567篇 |
大气科学 | 2349篇 |
地球物理 | 2639篇 |
地质学 | 4849篇 |
海洋学 | 1240篇 |
天文学 | 675篇 |
综合类 | 1023篇 |
自然地理 | 1112篇 |
出版年
2024年 | 27篇 |
2023年 | 126篇 |
2022年 | 373篇 |
2021年 | 425篇 |
2020年 | 355篇 |
2019年 | 441篇 |
2018年 | 459篇 |
2017年 | 446篇 |
2016年 | 565篇 |
2015年 | 450篇 |
2014年 | 570篇 |
2013年 | 551篇 |
2012年 | 526篇 |
2011年 | 525篇 |
2010年 | 633篇 |
2009年 | 532篇 |
2008年 | 527篇 |
2007年 | 491篇 |
2006年 | 375篇 |
2005年 | 379篇 |
2004年 | 284篇 |
2003年 | 299篇 |
2002年 | 273篇 |
2001年 | 335篇 |
2000年 | 344篇 |
1999年 | 548篇 |
1998年 | 475篇 |
1997年 | 435篇 |
1996年 | 441篇 |
1995年 | 373篇 |
1994年 | 315篇 |
1993年 | 305篇 |
1992年 | 252篇 |
1991年 | 199篇 |
1990年 | 152篇 |
1989年 | 128篇 |
1988年 | 129篇 |
1987年 | 66篇 |
1986年 | 60篇 |
1985年 | 45篇 |
1984年 | 31篇 |
1983年 | 24篇 |
1982年 | 38篇 |
1981年 | 31篇 |
1980年 | 20篇 |
1979年 | 17篇 |
1978年 | 7篇 |
1976年 | 8篇 |
1973年 | 5篇 |
1958年 | 18篇 |
排序方式: 共有10000条查询结果,搜索用时 828 毫秒
361.
本文计算了福建自1992年至2004年以来的地倾斜EW和NS两分量的固体潮潮汐因子,并进行动态组合,绘制组合动态三种特征量:ΔγEW ΔγNS(表征扩容)、ΔγEW-ΔγNS(表征剪切应变)、ΔγEW/ΔγNS(表征介质各向异性)的时序曲线图,并进行固体潮特征分析,寻找中、强地震发生前远场块体和近场块体地倾斜突变性形变异常与之对应关系。结果表明:在福建沿海,海潮是决定倾斜固体潮特征的主要因素;福建发生5级上的中强地震、台湾发生7级以上强烈地震时,福建地倾斜固体潮潮汐因子及其动态组合特征存在明显的渐进式突变性形变异常现象,异常量和异常持续时间与震级和震中距有较好的对应关系。 相似文献
362.
363.
我国公路泥石流病害严重,泥石流淤埋公路构建筑物是一类常见的公路泥石流病害类型。泥石流衰减动力学是防治泥石流淤埋病害的重要关键技术,也是泥石流运动学、动力学研究的核心问题之一。本文作者运用泥沙运动力学及流体力学原理,初步建立了泥石流固相颗粒和液相浆体的能量衰减条件,把泥石流衰减模式概化为两类,即能量抑制衰减和能量自由衰减;通过泥石流沉积模型试验,得到了不同粘度泥石流体的沉积扇变化形态,随着泥石流体粘度的增大,沉积扇边缘变陡、扩展范围变小、纵轴线长度减小等结论与实际情况吻合;初步建立了泥石流能量衰减速率计算方法。研究成果为防治公路泥石流病害奠定了基础。 相似文献
364.
Hydrochemical characteristics and salinity of groundwater in the Ejina Basin, Northwestern China 总被引:8,自引:0,他引:8
A hydrochemical investigation was conducted in the Ejina Basin to identify the hydrochemical characteristics and the salinity
of groundwater. The results indicate that groundwater in the area is brackish and are significantly zonation in salinity and
water types from the recharge area to the discharge area. The ionic ration plot and saturation index (SI) calculation suggest
that the silicate rock weathering and evaporation deposition are the dominant processes that determine the major ionic composition
in the study area. Most of the stable isotope δ18O and δD compositions in the groundwater is a meteoric water feature, indicating that the groundwater mainly sources from
meteoric water and most groundwater undergoes a long history of evaporation. Based on radioactive isotope tritium (3H) analysis, the groundwater ages were approximately estimated in different aquifers. The groundwater age ranges from less
than 5 years, between 5 years and 50 years, and more than 50 years. Within 1 km of the river water influence zone, the groundwater
recharges from recent Heihe river water and the groundwater age is about less than 5 years in shallow aquifer. From 1 km to
10 km of the river water influence zone, the groundwater sources from the mixture waters and the groundwater age is between
5 years and 50 years in shallow aquifer. The groundwater age is more than 50 years in deep confined aquifer. 相似文献
365.
Chemical weathering in the Upper Huang He (Yellow River) draining the eastern Qinghai-Tibet Plateau 总被引:8,自引:0,他引:8
We examined the fluvial geochemistry of the Huang He (Yellow River) in its headwaters to determine natural chemical weathering rates on the northeastern Qinghai-Tibet Plateau, where anthropogenic impact is considered small. Qualitative treatment of the major element composition demonstrates the dominance of carbonate and evaporite dissolution. Most samples are supersaturated with respect to calcite, dolomite, and atmospheric CO2 with moderate (0.710-0.715) 87Sr/86Sr ratios, while six out of 21 total samples have especially high concentrations of Na, Ca, Mg, Cl, and SO4 from weathering of evaporites. We used inversion model calculations to apportion the total dissolved cations to rain-, evaporite-, carbonate-, and silicate-origin. The samples are either carbonate- or evaporite-dominated, but the relative contributions of the four sources vary widely among samples. Net CO2 consumption rates by silicate weathering (6-120 × 103 mol/km2/yr) are low and have a relative uncertainty of ∼40%. We extended the inversion model calculation to literature data for rivers draining orogenic zones worldwide. The Ganges-Brahmaputra draining the Himalayan front has higher CO2 consumption rates (110-570 × 103 mol/km2/yr) and more radiogenic 87Sr/86Sr (0.715-1.24) than the Upper Huang He, but the rivers at higher latitudes are similar to or lower than the Upper Huang He in CO2 uptake by silicate weathering. In these orogenic zones, silicate weathering rates are only weakly coupled with temperature and become independent of runoff above ∼800 mm/yr. 相似文献
366.
GPS Solutions - The GPS satellite transmitter antenna phase center offsets (PCOs) can be estimated in a global adjustment by constraining the ground station coordinates to the current International... 相似文献
367.
368.
New magnetostratigraphic and pedostratigraphic investigations of loess deposits in north‐east China and their implications for regional environmental change during the Mid‐Pleistocene climatic transition
下载免费PDF全文
![点击此处可从《第四纪科学杂志》网站下载免费的PDF全文](/ch/ext_images/free.gif)
369.
370.
Q. Liu Y.‐B. Wu H. Wang S. Gao Z.‐W. Qin X.‐C. Liu S.‐H. Yang H.‐J. Gong 《Journal of Metamorphic Geology》2014,32(2):177-193
Migmatites are predominant in the North Qinling (NQ) orogen, but their formation ages are poorly constrained. This paper presents a combined study of cathodoluminescence imaging, U–Pb age, trace element and Hf isotopes of zircon in migmatites from the NQ unit. In the migmatites, most zircon grains occur as new, homogeneous crystals, while some are present as overgrowth rims around inherited cores. Morphological and trace element features suggest that the zircon crystals are metamorphic and formed during partial melting. The inherited cores have oscillatory zoning and yield U–Pb ages of c. 900 Ma, representing their protolith ages. The early Neoproterozoic protoliths probably formed in an active continental margin, being a response to the assembly of the supercontinent Rodinia. The migmatite zircon yields Hf model ages of 1911 ± 20 to 990 ± 22 Ma, indicating that the protoliths were derived from reworking of Palaeoproterozoic to Neoproterozoic crustal materials. The anatexis zircon yields formation ages ranging from 455 ± 5 to 420 ± 4 Ma, with a peak at c. 435 Ma. Combined with previous results, we suggest that the migmatization of the NQ terrane occurred at c. 455–400 Ma. The migmatization was c. 50 Ma later than the c. 490 Ma ultra‐high‐P (UHP) metamorphism, indicating that they occurred in two independent tectonic events. By contrast, the migmatization was coeval with the granulite facies metamorphism and the granitic magmatism in the NQ unit, which collectively argue for their formation due to the northward subduction of the Shangdan Ocean. UHP rocks were distributed mainly along the northern margin and occasionally in the inner part of the NQ unit, indicating that they were exhumed along the northern edge and detached from the basement by the subsequent migmatization process. 相似文献