地震与磁性基底起伏有很大的关系。
There may be close relation between magnetic basement characters and earthquakes.
本文通过分析和反演航磁异常场，研究了准噶尔盆地的磁性基底。
Through analysis and inversion of the aeromagnetic anomaly field, this paper has studied the magnetic basement of the Junggar basin.
用滑动对数能谱分析和人机交互正反演方法计算出磁性基底深度。
Using moving average of logarithmic energy and men-computer mutual system, the depth of magnetic basement was inversed.
揭示了延庆盆地、矾山盆地、怀来盆地、涿鹿盆地等四个相互联通盆地的磁性基底的定量特征。
The quantitative characteristics of the magnetic basement of the four correlative basins-Yanqing, Fanshan, Huailai and Zhuolu-are revealed.
研究表明，这一奇异的矫顽力特性与液相基底表面铁薄膜中的原子团簇尺寸分布、无序的薄膜表面磁各向异性以及团簇间的磁性相互作用等因素有关。
Our experimental results show that the anomalous magnetic properties are due to the non-uniform particle size distribution, random surface anisotropy and interparticle interactions in the films.
实验发现铁薄膜的生长过程与液相基底表面非磁性金属薄膜的情况类似，基本服从二阶段生长模型。
It is found that the growth mechanism of the iron films is similar to that of nonmagnetic films on liquid substrates, in accordance with a two-stage growth model.
实验发现铁薄膜的生长过程与液相基底表面非磁性金属薄膜的情况类似，基本服从二阶段生长模型。
It is found that the growth mechanism of the iron films is similar to that of nonmagnetic films on liquid substrates, in accordance with a two-stage growth model.
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