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381.
In this paper, based on the results of tomographic image of Tangshan and Xingtai areas, the relations between the characteristics of the two strong earthquake sequences and their three-dimensional velocity structures are studied. The research results indicate that:① Mosaic distribution of low-velocity bodies and high-velocity bodies, especially the existence of high-velocity bodies with large size in crust are the common basis of development of the two earthquake sequences. ②Scale, depth, and heterogeneity of high-velocity and low-velocity bodies are the important factors to effect the characteristic of earthquake sequences.③ The depth of the high-velocity body in Tangshan area is less than that in Xingtai area, which is the principal reason why the dominant focal depth and the biggest focal depth of Tangshan earthquake sequence are less than Xingtai's.④The depth of the high-velocity bodies in Ninghe area is more than that in Tangshan-Luanxian area, which lead to the biggest magnitude and epicentral intensity are lower. These results could be helpful for predicting the main shock of strong swarm-type earthquakes and later strong aftershocks. 相似文献
382.
“去干扰异常主分量门限化技术”,是在矿化蚀变异常提取和应用研究中形成的一套独具特色的方法技术,它使得大面积工程性的提取岩矿蚀变异常信息成为可能.该方法包括3个主要部分:预处理、信息提取和后处理技术,目前已经在PCI系统和ENVI系统上运行成功.经过笔者的反复试验,在Erdas系统中也成功地实现了该技术.将该技术运用到内蒙古查巴奇1:5万矿产调查中,取得了一定的成果,再次证明该方法的可行性. 相似文献
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384.
P. K. Das 《Journal of Astrophysics and Astronomy》1997,18(4):435-440
The variable Mass Hypothesis of conformal gravitation theory of Hoyle-Narlikar is used to develop a model for the anomalous
redshift quasar-galaxy associations. It is hypothesised that quasars are born in and ejected from the nuclei of parent galaxies
as massless objects and the particle masses in them systematically increase with epoch. The dynamics of such an ejection is
discussed and it is shown that the observed features such as redshift bunching and quasar alignments can be understood in
this scenario. Further tests of this hypothesis are suggested. 相似文献
385.
The Mössbauer spectra of one chromite at 298 K and one chromite at 298, 200, 170, 140 and 90 K have been analyzed in this study. A Voigt-based quadrupole splitting distribution (QSD) method was used to analyze the spectra. The tetrahedral site Fe2+ and the octahedral site Fe3+ quadrupole splitting distributions (QSDs) were obtained from the Mössbauer spectra of chromites, and the multiple tetrahedral site Fe2+ Gaussian QSD components and the large widths σ Δ of the Gaussian QSD components of the tetrahedral site Fe2+ QSDs for chromites were attributed to next-nearest neighbor effects. In addition, temperature dependences of the isomer shift and the quadrupole splitting were presented and discussed. Comparisons between the Mössbauer parameters for thickness-corrected folded spectra and raw-folded spectra of chromites were made, and the results show that the two sets of the Mössbauer parameters and ratios of ferric to total iron as well as χ2 are very close to each other. This is because of the small absorber thickness of chromites in this study. Comparisons between the Mössbauer parameters of chromites obtained using the Voigt-based QSD method and a Lorentzian doublet method were also made. The results show that there are some differences between the two sets of the Mössbauer parameters and ratios of ferric to total iron, but not significant. However, much larger χ2 were obtained when the Lorentzian doublet method was used to fit the spectra of chromites. This indicates that the Voigt-based QSD method is more adequate to analyze the Mössbauer spectra of chromites from the point of view of statistics. 相似文献
386.
金矿床定年方法进展及研究现状 总被引:10,自引:1,他引:10
热液蚀变矿物,流体包裹体,脉石英,水热锆石和某些矿石矿物同位素定年方法的新进展使金矿床定年精度大大提高。热释发光等新技术区分成矿前或成矿后脉岩,异常铅模型研究可有效地示踪金矿化历史,在坚实的成矿背景和矿床地质地球化学基础上,采用多元同素体系结构分析是今后矿床定年的主要方向。 相似文献
387.
1976年唐山7.8级地震前气象要素的异常变化 总被引:2,自引:0,他引:2
系统研究了唐山地震前气象要素的异常变化。地震前约一个月时间,震中及附近地区月平均气压变化幅度最大,月平均气压距平中心区域与震中区吻合,沿区域构造带方向出现气压变化最大梯度区,临震前几天气民较大幅度的升、降变化过程,升压脊 区域构造瞳向吻合。地震前一年,丰润、唐山一带年平均气温距平值最大,地震前一天,气温24小时变温的升温中心在唐山,升温脊受区域构造带控制。0.8m地温亦有明显的升温异常变化。197 相似文献
388.
对大同-阳高地震的地磁场△F时、空变化做了分析。认为6.1级地震前8个月山西北部地磁场△F出现异常,同年9月达高潮。6.1级地震后的1990年3月地磁场活动又出现了第2次高潮。2次高潮的异常幅度分别为13.0nT和13.2nT。大同-阳高地震的地磁异常具有时段长,连续性好,空间分布广的特点。 相似文献
389.
390.