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1.
王非  周新华 《地球学报》1997,18(Z1):126-128
本文通过对辽西及邻区中生代盆地火山岩稀土元素配分特征的研究及模拟运算,探讨了其岩浆成因及过程。结果显示南北岩区岩浆成因不同,南岩区岩源为MORB地幔和长期富集型幔熔融混合而成,北岩区为MORB和近期亏损型地幔熔融混合而成。  相似文献   
2.
匡亮  仇文革 《岩土力学》2006,27(Z1):524-528
详细地介绍了曲墙式、直墙式和圆形断面隧道衬砌在约束条件、隔热保温层及含水状况等因素变化情况下的相似材料冻胀力室内模型试验,通过分析试验得出不同衬砌断面在各种因素影响下衬砌和围岩间冻胀压力的量值和分布特征,以及由冻胀压力引起的结构内力分布特征。研究表明,直墙式断面受冰胀力最大,曲墙式次之,圆形面最小;曲墙式、直墙式断面冻胀力均呈分布荷载形态,前者拱脚及仰拱脚处冻胀力最大,后者边墙、底板处冻胀力最大。  相似文献   
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Dunhuang Yardang National Geo-park,situated in the Gansu Province of northwestern China(40o25'36 "N–40o33'10" N,93o00'00 "E–93o13'30" E),was chosen as a research locality of aesthetics evaluation of yardang landforms landscape.The yardang landforms landscape is a composite structural system of patch-corridor-matrix,with four landscape unit elements as dense group,sparse group,single body and remnant.The study of the landscape aesthetics spatial pattern of Dunhuang Yardang National Geo-park shows that yardang dense group,sparse group and single body provide the greatest contribution to the aesthetic value of yardang landforms landscape.Yardang bodies are scarce,unique,irreplaceable,and priceless resources in yardang landforms areas.However,they are easily destroyed under the influence of the natural and artificial factors.Therefore,when the tourism potential of yardang landforms landscape is exploited,the protection should be fully improved.  相似文献   
5.
未来全球气候变化是人们关注的重大课题。从内蒙古盐湖近20ka气候演变的研究可知,地质时期和历史时期气候波动变化是有规律可循的。用已经了解的这种变化规律来予测未来气候变化是有价值的。研究表明,未来1ka左右全球为暖期,之后将进入下一个冰期。  相似文献   
6.
Sanjiang and Jiaodong areas are the important gold regions in China. The gold mineralization is cor- related with the Mesozoic faults and its derivative faults in the granite or the contact zone between granite and base rock. The mineral mapping is one of the important approaches of prospecting mineralogy. The temporal and spatial band distribution of mineral, mineral combination and mineral typomorphism features are natural regularity rules, but this kind of band feature is sometimes hidden and thus in need of mineral typomorphism re- search and mapping to disclose this band feature and to serve for the prospecting of mineral. The changes of the mineral typomorphism feature are often embodied in the " through" mineral, the typomorphism features of the through mineral change like the gradient toward the ore body, and the changes of the features are most obvious and strongest toward the orebodies. The new American mineralogy mapping indicates the weak change of the mineral composition or structure will lead to the change of the shape and wave length position of the specific ab- sorbent feature. Australian experiment lab investigation has held the reason of a series of mineral. The progress achievement of the remote sensing and computer analysis technology now permits a direct comparison directly between the lab and remote sensing data, so the good feature database of the experiment light spectroscopy can serve for drawing of the spacial distribution and remote sensing material. Mineralogy mapping raised the exten- sive emphasis in the international earth arena.  相似文献   
7.
We have determined the production yields for radionuclides in Al2O3, SiO2, S, Ar, K2SO4, CaCO3, Fe, Ni and Cu targets, which were irradiated with slow negative muons at the Paul Scherrer Institute in Villigen (Switzerland). The fluences of the stopped negative muons were determined by measuring the muonic X-rays. The concentrations of the long-lived and short-lived radionuclides were measured with accelerator mass spectrometry (AMS) and γ-spectroscopy, respectively. Special emphasis was put on the radionuclides 10Be, 14C and 26Al produced in quartz targets, 26Al in Al2O3 and S targets, 36Cl in K2SO4 and CaCO3 targets, and 53Mn in Fe2O3 targets. These targets were selected because they are also the naturally occurring target minerals for cosmic ray interactions in typical rocks. We also present results of calculations for depth-dependent production rates of radionuclides produced after cosmic ray μ capture, as well as cosmic ray-induced production rates of geologically relevant radionuclides produced by the nucleonic component, by μ capture, by fast muons and by neutron capture.  相似文献   
8.
本文首先概述了新城子地电阻率的观测环境,并根据新城子台近年几次地电阻率的异常变化,通过理论分析和观测环境实际凋杏,发现了铁栅栏、大气降水、观测室改造等干扰因素,分析了各种干扰曲线形态,为今后地电阻率干扰识别和排除提供参考。  相似文献   
9.
Rare earth elements (REEs) in the suspended particulate matter (SPM) of the Mandovi estuary indicated that the mean total-REEs (∑REE) and light REE to heavy REE ratios are lower than that of the average suspended sediment in World Rivers and Post-Archean average Australian shale. High ∑REE were associated with high SPM/low salinity and also with high SPM/high salinity. Although the ∑REE broadly agree with SPM levels at each station, their seasonal distributions along transect are different. SPM increased seaward in the estuary both during the monsoon and pre-monsoon, but consistently low at all stations during the post-monsoon. The mean ∑REE decreased marginally seaward and was <25% at sea-end station than at river-end station. Spatial variations in ∑REE are maximum (64%) during the pre-monsoon. Strong to moderate correlation of ∑REE with Al, Fe and Mn in all seasons indicates adsorption and co-precipitation of REEs with aluminosilicate phases and Fe, Mn-oxyhydroxides. The ratio of mean ∑REE in sediment/SPM is low during the monsoon (1.27), followed by pre-monsoon (1.5) and post-monsoon (1.62). The middle REE- and heavy REE-enriched patterns with positive Ce and Eu anomalies are characteristic at every station and season, both in SPM and sediment. They also exhibit tetrad effect with distinct third and fourth tetrads. Fe-Mn ore dust is the most dominant source for REEs. However, the seasonal changes in the supply of detrital silicates, Fe-Mn ore dust and particulates resuspended from bottom sediments diluted the overall effect of salinity on fractionation and distribution of REEs in the estuary.  相似文献   
10.
中国中老年人红细胞压积参考值与地理因素的关系   总被引:1,自引:1,他引:1  
葛淼 《地理科学》1999,19(1):78-81
海拔高度是影响中老年人红细胞压积参考值最主要的因素,随着海拔高度的逐渐增大,中老年人红细胞压积参考值也在逐渐增大,相关性很显著,用逐步回归分析的方法推导出二个回归方程,依据中老年人红细胞压积参考值与地理因素的依赖关系把中国分为青藏区,西南区,西北区,东南区,华北区,东北区等6个区。  相似文献   
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