全文获取类型
收费全文 | 23631篇 |
免费 | 4254篇 |
国内免费 | 5752篇 |
专业分类
测绘学 | 1757篇 |
大气科学 | 4601篇 |
地球物理 | 6298篇 |
地质学 | 11759篇 |
海洋学 | 3459篇 |
天文学 | 935篇 |
综合类 | 2199篇 |
自然地理 | 2629篇 |
出版年
2024年 | 138篇 |
2023年 | 518篇 |
2022年 | 1137篇 |
2021年 | 1340篇 |
2020年 | 1093篇 |
2019年 | 1171篇 |
2018年 | 1268篇 |
2017年 | 1235篇 |
2016年 | 1357篇 |
2015年 | 1182篇 |
2014年 | 1430篇 |
2013年 | 1508篇 |
2012年 | 1367篇 |
2011年 | 1363篇 |
2010年 | 1418篇 |
2009年 | 1301篇 |
2008年 | 1107篇 |
2007年 | 1200篇 |
2006年 | 904篇 |
2005年 | 828篇 |
2004年 | 577篇 |
2003年 | 628篇 |
2002年 | 642篇 |
2001年 | 596篇 |
2000年 | 708篇 |
1999年 | 1027篇 |
1998年 | 885篇 |
1997年 | 838篇 |
1996年 | 799篇 |
1995年 | 737篇 |
1994年 | 641篇 |
1993年 | 538篇 |
1992年 | 448篇 |
1991年 | 322篇 |
1990年 | 258篇 |
1989年 | 214篇 |
1988年 | 204篇 |
1987年 | 117篇 |
1986年 | 123篇 |
1985年 | 80篇 |
1984年 | 61篇 |
1983年 | 63篇 |
1982年 | 59篇 |
1981年 | 41篇 |
1980年 | 47篇 |
1979年 | 36篇 |
1978年 | 17篇 |
1977年 | 11篇 |
1974年 | 9篇 |
1958年 | 18篇 |
排序方式: 共有10000条查询结果,搜索用时 1 毫秒
81.
An update on the IEM surface backscattering model 总被引:1,自引:0,他引:1
The integral equation approach to modeling scattering from rough surfaces was introduced in 1992. At that time, it was noted that there was a need to find a transition reflection coefficient that could change its argument from the incident angle to the specular angle as frequency or roughness scale got large. One such reflection coefficient was published in 2001. In this letter, we would like to include this reflection coefficient in the integral equation model to interpret several multifrequency backscattering measurements from surfaces with surface parameters defined by the investigators who acquired the data. 相似文献
82.
83.
铜陵地区老鸦岭层状钼矿床铅同位素组成研究 总被引:1,自引:0,他引:1
安徽铜陵老鸦岭矿床中二叠系大隆组(P2d)顶部的含矿(钼矿化)黑色页岩以及附近(立新煤矿)同一层位不含矿黑色页岩的实测铅同位素组成分别为:^206Pb/^204Pb20.20~22.37,^207Pb/^204Pb15.67~15.82,^208Pb/^204Pb38.47~38.60和^206Pb/204Pb18.83~20.80,^207Pb/^204Pb15.65~15.76,^208Pb/^204Pb38.84~39.22。对137Ma的放射成因Pb进行校正后的铅同位素组成表明,含矿黑色页岩和不含矿黑色页岩均与燕山晚期火成岩无关,老鸦岭含矿黑色页岩可能具沉积成因。对沉积(约250Ma)以来的放射成因Pb进行校正后的铅同位素组成表明:不含矿黑色页岩的Pb源自上地壳,而含矿黑色页岩的Pb(因而推测其他成矿金属)可能源于上地壳物质(与不含矿黑色页岩的Pb源相似)与下地壳物质的混合。 相似文献
84.
碳酸岩Sr、Nd、Pb 同位素地球化学研究评述 总被引:3,自引:0,他引:3
碳酸岩是出露相对较少的幔源岩石,其中Sr与Nd是研究地幔物质组成的主要对象之一。本文统计了世界上主要碳酸岩的锶、钕、铅同位素组成特征;研究显示,碳酸岩源区主要是洋岛玄武岩高U/Pb的HIMU端员和富集端员(EM1或EM2)的混合作用;此外大部分碳酸岩的锶、钕同位素落在大洋玄武岩范围内;这些均表明其成因与地慢柱有密切联系。碳酸岩及与之共生的硅酸岩的同源或独立源区模式部很难充分解释两者同位素组成特征,逭反映碳酸岩的演化模式涉及更复杂的过程。可能是俯冲作用使碳酸岩源区经历不同时间和程度的富集、亏损过程导致地幔源区成分不均一。 相似文献
85.
论述了用瑞利波检测高速公路软基加固的一些主要技术问题,应用新兴的小波分析技术,改善和提高检测的质量,并通过福宁高速公路的实际检测结果,说明了其思路和方法的正确性、实用性. 相似文献
86.
ZHAO Pengda 《中国地质大学学报(英文版)》2004,15(3):245-252
“Three-component” method consists of three clase-connected aspects: geological anomaly,diversity of mineralization and mineral deposit spectrum. All these three concepts are not new separately, but it is a new approach to combine these three aspects in one single concept for quantitative mineral resources prediction and assessment and it is also the first time to conduct a more detailed study in each aspect. Investigation and clarification of geological anomalies, diversity of mineralization and spectrum of mineral deposits are realized by digitization and quantification of ore forming controlling factors, oreexisting symbols or marks, characteristics of mineralization and regulation of ore-genesis and laws of distribution. These procedures lead to construction of a “digital model“ for mineral resources prediction andassessment. 相似文献
87.
Asynchronous Holocene climatic change across China 总被引:1,自引:0,他引:1
A review of Holocene climatic variations in different parts of China shows that they were asynchronous. Proxy data from ice cores, pollen, loess, lacustrine sediments, and changes of sea and lake levels demonstrate that many warm and cold oscillations have occurred in China during the Holocene, including a most important climatic event known as the “Holocene optimum,” a milder and wetter period, and that the duration and amplitude of the optimum period, as well as its start and end times, differed in different parts of China. Uplift of the Tibetan plateau over the past millions of years led to the development of the monsoon climate and to complex atmospheric circulation over continental China during the Holocene. As a result, the Holocene optimum began and terminated earlier in high-altitude regions of western China than at lower elevations in eastern China, and the amplitude of the variations was lower in the east. This suggests that the western higher-altitude areas were more sensitive to climatic change than were the eastern lower-altitude areas. Holocene climatic records in the Dunde and Guliya ice cores do not correspond. Inverse δ18O variations between the two cores indicate that the effects of climate and atmospheric processes on the stable isotopes at the two sites differed. The correlation between the isotopic composition of carbonates in lake deposits in western China and climatic variations is similar to that in the ice cores. The climatic resolution in ice cores and lake sediments is higher than that in other media. The lack of precise correspondence of climatic records constructed on the basis of proxy data from different parts of China is a result of the different locations and elevations of the sampling sites, the different resolutions of the source material, and the varied climatic conditions within China. Further work is needed to confirm both the conclusions and the inferences presented here. 相似文献
88.
Chen-Tung Arthur Chen Jiunn-Tzong Wu Bing-Jye Wang Kuo-Ming Huang 《Aquatic Geochemistry》2004,10(1-2):33-57
One hundred and eighty lakes, ponds and reservoirs in Taiwan, and the offshore islands have been investigated since 1985. Effects such as warming/cooling, mixing, photosynthesis and respiration on pH have been identified. These effects were found to be less profound than those resulting from the geology. Since there is little rain or lake water pH data available prior to 1970, it was necessary to use proxy data in order to ascertain the history of lake acidification. In this study, we present data based on diatoms in a sediment core collected from a lake in the remote subalpine region of southern Taiwan. The acidity of this lake water was found to have increased since 1900. We measured the concentrations of 55 chemical species in lake water samples. In addition, concentrations of 26 chemical species were obtained from sediments. Conductivity, alkalinity (HCO3 ?), most other major and minor chemical species, as well as the non sea-salt SO4/Na ratio in lake water clearly decrease with elevation. Distribution of pH is similar, although the trend is less clear. Distribution of trace metals, however, shows a different trend as anthropogenic pollution, diagenetic reduction and lake acidification are at play. 相似文献
89.
90.