It indicated that the geomagnetic anomaly is a promising phenomenon in the studies of earthquake precursors.
说明地磁异常变化是一种有希望的地震前兆现象。
ANOMALOUS VARIATION OF REGIONAL GEOMAGNETIC FIELD BEFORE THE BOHAI SEA EARTHQUAKE (7.4M_S)
渤海7.4级地震前区域地磁场的异常变化
Anti-phase Phenomena on Two Sides of Geomagnetic Low-point Displacement Line and Its Interpretation
地磁低点位移线两侧异常变化的反相位现象及其解释
The forward modeling of Transient Electromagnetic method to 3D Body with Topography
瞬变电磁法对含地形的三维异常体的正演计算
POSSIBLE ANOMALOUS CHANGES OF GEOMAGNETIC TRANSFER FUNCTIONS AT HEZE STATION RELATED TO THE M5.9 HEZE EARTHQUAKE OF NOV. 7, 1983
与1983年11月7日菏泽5.9级地震可能有关的菏泽台地磁转换函数异常变化
The strength and the center position of each above magnetic anomaly changed with time, and the trend of each change is not alike.
各个磁异常的强度和中心位置随时间变化 ,变化趋势各不相同 .
Middle Cretaceous abnormal geological events and global change
白垩纪中期异常地质事件与全球变化
The "double low-points" anomaly of daily vertical component variation of geomagnetic field before the M8.0 Wenchuan earthquake
汶川8.0级特大地震前的地磁垂直分量日变“双低点”异常
The Geologic Interpretation Research of Double-magnetism Anomaly and Negative Magnetism Anomaly Zone in Qing-Tibet Plateau;
青藏高原航磁双磁异常带与负磁异常区地质意义研究
Analysis of Anomalous Character and Study Vector Intersection for Downhole Transient Electromagnetic Method
地—井瞬变电磁异常特征分析及矢量交会解释方法研究
Therefore, it is possible to predict earthquake using asynchronous variation of amplitude difference of daily change.
从而提出利用地磁日变幅差的异步变化现象预报地震的可能性。
Recent Time-Space Dynamic Evolution Characteristics of Geomagnetic Field in Jiangsu-Shandong-Henan-Anhui Region
苏鲁豫皖地区地磁异常场时空近期动态演化特征
It may be infeasible to say whether an observed magnetic anomaly results from structural relief or from a lateral change in susceptibility.
不可能指出一个观测磁异常是构造起伏还是磁化率的横向变化所引起。
Response Analysis of the Earth Electromagnetism Exceptionally in Earthquake Process
地震过程中的大地电磁异常响应关系
Three-Dimensional Anomalous Characteristics Inversion of Fixed Loop Source Transient Electromagnetic Method;
定回线源瞬变电磁三维异常特征反演
Signal Variability in MR Imaging of Normal Adult Hip
正常成人股骨头的磁共振成像及变异
Joint Inversion of Gravity and Magnetic Data with Varying Density and Constant Magnetic Susceptibility Interface Model
变密度常磁化强度界面重磁联合反演
The geomagnetic field varies continuously.
地磁场不断地发生变化。