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characteristics of anomalies
相关语句
  异常特征
    Study on characteristics of anomalies near by epicenter of Zhangbei M_s6.2 earthquake and their spatial and temporal evolution
    张北6.2级地震近震区前兆异常特征及时空演化研究
短句来源
    In this paper,the relation between the characteristics of anomalies of groundwater level immediately before earthquake and earthquakes is preliminarily expounded, and meanwhile their formation mechanism is discussed.
    本文初步阐述了地下水位临震异常特征及其与地震的关系,同时探讨了它的形成机理。
短句来源
    Based on distribution characteristics of anomalies of underground fluids and gravity in the North China, the features of deep seated material and stress field in the shallow crust before and after main earthquakes are discussed combining the geophysical prospecting data.
    :根据华北几次强震前后地下流体和重力异常特征 ,结合大地测深资料探讨了地震发生前后深部介质的变化和地壳浅层应力场变化特征。
短句来源
    The characteristics of anomalies for all the data of earth resistivity during the three earthquake groups occurred in North China (Tangshan group occurred in 1976, Datong group occurred in 1989, Zhangbei group occurred in 1998) are analyzed.
    分析了自有地电阻率观测资料以来华北地区发生的三次成组地震前后的异常特征,其中包括1976年唐山地震组、1989年大同地震组和1998年张北地震组。
短句来源
  异常特征
    Study on characteristics of anomalies near by epicenter of Zhangbei M_s6.2 earthquake and their spatial and temporal evolution
    张北6.2级地震近震区前兆异常特征及时空演化研究
短句来源
    In this paper,the relation between the characteristics of anomalies of groundwater level immediately before earthquake and earthquakes is preliminarily expounded, and meanwhile their formation mechanism is discussed.
    本文初步阐述了地下水位临震异常特征及其与地震的关系,同时探讨了它的形成机理。
短句来源
    Based on distribution characteristics of anomalies of underground fluids and gravity in the North China, the features of deep seated material and stress field in the shallow crust before and after main earthquakes are discussed combining the geophysical prospecting data.
    :根据华北几次强震前后地下流体和重力异常特征 ,结合大地测深资料探讨了地震发生前后深部介质的变化和地壳浅层应力场变化特征。
短句来源
    The characteristics of anomalies for all the data of earth resistivity during the three earthquake groups occurred in North China (Tangshan group occurred in 1976, Datong group occurred in 1989, Zhangbei group occurred in 1998) are analyzed.
    分析了自有地电阻率观测资料以来华北地区发生的三次成组地震前后的异常特征,其中包括1976年唐山地震组、1989年大同地震组和1998年张北地震组。
短句来源
  “characteristics of anomalies”译为未确定词的双语例句
    The spatial and temporal characteristics of anomalies nearby epicenter (△≤200 km) show that anomalies occurred in groups and by stages, reflecting the strengthening process of field stress.
    在汇总首都圈及其周围地区各种前兆异常的基础上,研究了近震区(200km范围内)前兆异常的空间、时间演化特征。 结果表明,前兆异常的发展过程存在较明显的阶段性和成组性,反映了震前区域应力场的增强过程。
短句来源
    The characteristics of anomalies and the relation between these anomalies and the earthquake are discussed here.
    本文对这些异常的特征进行了分析,同时讨论了这些异常和这次地震的关系。
短句来源
    While the forward models figure and energy figure with wide band signal as the transmitting source only to be able approximately to see the air-soil minute contact surface,cannot distinguish the anomalies,and its corresponding energy figures have many irregular pulses which can't reflect the shape and position characteristics of anomalies.
    而宽带信号作为发射源的正演模型只能大致看出空气土壤分界面,不能较好地分辨出异常体,其相应的能量图具有不规则的多个脉冲,也不能反映异常体的形状位置特征。
短句来源
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In this paper,the relation between the characteristics of anomalies of groundwater level immediately before earthquake and earthquakes is preliminarily expounded, and meanwhile their formation mechanism is discussed.

本文初步阐述了地下水位临震异常特征及其与地震的关系,同时探讨了它的形成机理。

In this paper, the statisties and analysis of the variations of 189 observed items after the Tangshan M7. 8 earthquake have been made, the relation between the differential characteristics of 5 kinds of variations in quantity after the earthquake and the follow - up earthquakes has been discussed, the corresponding relation between the distribution characteristics of anomalies after the earthquake and the follow-up seismic area and anomalous seismic activity has been analyzed. It is considered that using...

In this paper, the statisties and analysis of the variations of 189 observed items after the Tangshan M7. 8 earthquake have been made, the relation between the differential characteristics of 5 kinds of variations in quantity after the earthquake and the follow - up earthquakes has been discussed, the corresponding relation between the distribution characteristics of anomalies after the earthquake and the follow-up seismic area and anomalous seismic activity has been analyzed. It is considered that using some comprehensive characteristics of the precursors after earthquake, coordinating seismomitry method, to make tendency prediction is of practical value.

本文对唐山7.8级地震各前兆学科共189个测项的震后变化进行了归类统计与分析,讨论了震后变化的5种类型数量上的差异特征与后续地震的关系,分析了震后异常的分布特征与后续地震区及其地震活动异常的对应关系,认为利用前兆学科的震后变化的某些综合特征配合测震学进行震后趋势判断有实用价值.

The seismicity map of 1990 Changsu-Taicang Ms5. 1 earthquake shows an undulation,belt and small groups forms. Groundwater anomalies are located almost along the normsl direction of rupture plane instead of direction of fracture zone. These anomalies can be explained by the IPE modal. The space distribution characteristics of anomaly is important tothe research of earthquake prediction.The lunar eclipse occured over Changsu may be a trigger factor half hour before theearthquake.

这次地震前震中附近地区的地震活动随时间呈波浪式起伏,形成了小震条带,出现了小震群;地下水(水位、水温)异常非常强烈;地形变异常也观测到了。分析发现:前兆不是沿断裂带分布,而主要是于近震中(≤50km)的破裂面法线方向;似可用IPE模式解释一些前兆现象。地震前兆的空间分布对未来震中的预报是很有意义的。震前半小时发生的,位于震中地区上中天的月蚀或许触发了这次地震。必须指出的是本文所采用的异常都是在震前发现的。

 
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