全文获取类型
收费全文 | 8685篇 |
免费 | 2272篇 |
国内免费 | 2963篇 |
专业分类
测绘学 | 388篇 |
大气科学 | 1667篇 |
地球物理 | 2147篇 |
地质学 | 6258篇 |
海洋学 | 968篇 |
天文学 | 79篇 |
综合类 | 1139篇 |
自然地理 | 1274篇 |
出版年
2024年 | 44篇 |
2023年 | 133篇 |
2022年 | 283篇 |
2021年 | 335篇 |
2020年 | 339篇 |
2019年 | 442篇 |
2018年 | 392篇 |
2017年 | 446篇 |
2016年 | 443篇 |
2015年 | 505篇 |
2014年 | 616篇 |
2013年 | 609篇 |
2012年 | 696篇 |
2011年 | 707篇 |
2010年 | 655篇 |
2009年 | 688篇 |
2008年 | 619篇 |
2007年 | 689篇 |
2006年 | 679篇 |
2005年 | 578篇 |
2004年 | 487篇 |
2003年 | 437篇 |
2002年 | 389篇 |
2001年 | 400篇 |
2000年 | 317篇 |
1999年 | 328篇 |
1998年 | 287篇 |
1997年 | 246篇 |
1996年 | 208篇 |
1995年 | 173篇 |
1994年 | 147篇 |
1993年 | 147篇 |
1992年 | 105篇 |
1991年 | 83篇 |
1990年 | 64篇 |
1989年 | 47篇 |
1988年 | 44篇 |
1987年 | 25篇 |
1986年 | 15篇 |
1985年 | 14篇 |
1984年 | 6篇 |
1982年 | 4篇 |
1981年 | 5篇 |
1980年 | 10篇 |
1979年 | 5篇 |
1978年 | 11篇 |
1977年 | 13篇 |
1976年 | 1篇 |
1972年 | 1篇 |
1954年 | 2篇 |
排序方式: 共有10000条查询结果,搜索用时 31 毫秒
701.
本矿物为新发现的钇易解石族的端员矿物-钛钇易解石,产于江西省龙南县足洞燕山期中粒白云母花岗岩及其风化壳中。矿物属斜方晶系,常呈板状或短柱状,为天然晶质体,浅黄色,粒度为0.075mm,硬度4.7,比重4.73,二轴正晶,Ng=2.248,Nm=2.212,Np=2.194,Ng-Np=0.054,2V=70°。空间群为D^162h-Pmnb,a0=0.750nm,b0=1.092nm,C0=0.5 相似文献
702.
Yutaka Ishizaka Peter V. Hobbs Lawrence F. Radke 《Journal of Atmospheric Chemistry》1989,9(1-3):149-159
Airborne measurements made during August 1985 over Greenland and its environs show that both accumulation-mode (0.1 m D2.0 m) and giant (D2 m) particles were present in relatively high concentrations in arctic haze layers and that the accumulation-mode particles dominated light scattering. Particles with diameters (D) between 1 and 4 m consisted predominately of mixed materials, small and dense inclusions, and probably organic compounds containing sulfur. Many of the particles from 0.1 to 1 m in diameter were also of mixed composition, with sulfuric acid, ammonium sulfate and organics probably the dominant constituents. 相似文献
703.
Temporal variations in bedload transport rates that occur at a variety of timescales, even under steady flow conditions, are accepted as an inherent component of the bedload transport process. Rarely, however, has the cause of such variations been explained clearly. We consider three data sets, obtained from laboratory experiments, that refer to measurements of bedload transport made with continuously recording bedload traps. Each data set is characterized by a predominant low-frequency oscillation, on which additional higher-frequency oscillations generally are superimposed. The period of these oscillations, as isolated through the use of spectral analysts, ranged between 0·47 and 168 minutes, and was associated unequivocally with the migration of bedforms such as ripples, dunes, and bars. The extent to which such oscillatory behaviour may be recognized in a data set depends on the duration of sampling and the length of the sampling time, with respect to the period of a given bedform. Several theoretical probability distribution functions have been developed to describe the frequency distributions of (relative) bedload transport rates that are associated with the migration of bedforms (Einstein, 1937b; Hamamori, 1962; Carey and Hubbell, 1986). These distribution functions were derived without reference to a sampling interval. We present a modification of Hamamori's (1962) probability distribution function, generated by Monte Carlo simulation, which permits one to specify the sampling interval, in relation to the length of a bedform. Comparisons between the simulated and observed frequency distributions, that were undertaken on the basis of the data described herein, are good (significant at the 90 per cent confidence level). Finally, the implications that temporal variability, which is associated with the migration of bedforms, have for the accurate determination of bedload transport rates are considered. 相似文献
704.
705.
The major chemical components of bauxite deposits of Belgaum (76° 24′E : 15° 54′N) and Yercaud (78° 14′E : 11° 48′N) areas
have been determined. A chemical continuity between parent rocks (zone I) to bauxites (zone IV) via clay (zone II) and laterites
(zone III) clearly indicates that bauxites have been derived byin situ weathering of the respective parent rocks. 相似文献
706.
本文探讨了矿物热释氡找矿中氡的来源问题。我们对七五二花岗岩中铀矿床的无矿及含矿花岗岩用闪烁射气法进行了各种温度间的矿物热释氡量的测定;用包裹体爆裂法进行了爆裂温度及相对爆裂次数的测定。通过实验发现,加热样品在包裹体爆裂以前,能释放出大部分氡,在包裹体大量爆裂的温度区间热释氧量反而很少。磨破包裹体放出氡后,再加热仍然有氡气释放出来。用包裹体中的铀含量计算出的氡量低于测定方法的灵敏度,无法测出,说明矿物热释氡量与包裹体无关。样品又做了化学铀分析和放射化学镭分析。明显看出热释氡量与铀、氡含量成正相关关系。各种实验均证明氧气不是来自包裹体,而是来源于整个矿物。 相似文献
707.
本文总结了706矿点水中放射性元素的富集、迁移、分布特点及其与水的化学成分的关系,作者评价了该区放射性水异常的铀成矿远景,并进一步指导了水化学找矿工作。另外,根据该矿点的水文地质条件和氡的迁移规律,定量预测了盲矿体赋存的空间位置。 相似文献
708.
在我国东部沿海修建地下水封石洞油库若干问题的探讨 总被引:2,自引:0,他引:2
随着我国大陆架油、气田不断被发掘、开采,石油储运问题已指日可待。我国海岸线的基岩岸约占全长的2/3以上,其中,块状结晶岩体又占基岩岸的一半以上,这就给水封油库的布置提供了良好的基础。在油库的选择和兴建中,应加强对建库岩体和主要结构面、地应力及其分布的充分研究,以期能对洞库稳定问题、地下水位及水量的合理确定问题有所裨盖、 相似文献
709.
Two hydrogen-rich lithobodies of highly alipathic character from a coal occurring in southwest Utah, have been studied. Bituminite (>50%), vitrinite (25–30%) and liptodetrinite (7–12%) are the principal macerals. The hexane-soluble products of hydrogenating the lithotypes at 400° with tetralin and hydrogen have been analyzed by GC-MS. Products identified include homologous series of alkylated naphthalenes, phenols, furans, cyclohexenones and hydroxy-pyridines. In the case of furans, the alkyl groups extend beyond C30. Materials released by Soxhlet extraction with pyridine consist chiefly of homologous series of fatty acids and their methyl esters and of methyl alkyl ketones, which were not found in the hydrogenation products. The long alkyl chains in these substances can account for about 75% of the alkanes found in the hydrogenation products but not in the extracts. Most of the compounds mentioned in the foregoing are thought to be physically held or trapped in the coal, rather than chemically combined in its macromolecular network. Except for the fatty acids, the origins of these substances are difficult to identify. 相似文献
710.
Mine ventilation planning in the 1980s 总被引:1,自引:0,他引:1
Malcolm J. Mcpherson 《Geotechnical and Geological Engineering》1984,2(3):185-227
Conclusions In this paper, the author has attempted to trace the development of mine ventilation planning from the traditional, manual and largely empirical methods of the past to the numerate computer-based techniques of the 1980s.The computer revolution has changed the face of many engineering disciplines, not least mine environmental engineering. Nevertheless, the mining industries of the world have not all been equally progressive in adapting to the flexibility, power and practical utilization of the new methodologies. It is, for example, incongruous that current textbooks on mine ventilation separate completely the topics of network analysis and ventilation planning with very little cross-referencing. Many of the current generation of mine ventilation engineers recognize the need to know about computers but find difficulty in translating this into their daily work. The growing availability of self-teaching, friendly software for personal microcomputers, coupled with interactive graphics, will assist greatly in promoting uncomplicated but powerful usage of computers.Young engineers now graduating from universities and colleges have been brought up in a computer-oriented environment and are competent in interacting with these machines. Indeed, they wonder how the job was ever done without magnetic data bases and high-speed computation aid. 相似文献