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地磁低点位移线两侧异常变化的反相位现象及其解释 总被引:5,自引:2,他引:3
本文通过部分震例研究发现,在地磁低点位移异常日及附近,分布于低点位移线两侧的地磁垂直分量日变化畸变异常部分具有反相位变化特征,而水平分量无类似的现象.作者依据Biot-Savart定律推测,在低点位移异常期间,在低点位移线下方有一引起地磁垂直分量日变化畸变的电流通过,且该电流为线状分布,或仅在垂直面内有分布,埋深一般认为几十千米.作者同时分析认为,当这种电流的分布形成闭合圈或有东西分量时,地磁基本场对其产生的作用力对地震的发生可能有触发作用. 相似文献
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地磁幅相法中的年变消除及在常熟Ms5.1地震前兆分析中的应用 总被引:2,自引:1,他引:2
地磁幅相法的瞬时差幅度与地磁2分量日变幅差值一样具有年变规律,应在分析震前异常时消除,并视被处理资料长度及在年变周期中所处的位置,采取不同方法消除年变。应用线性去倾技术处理了1990年2月10日江苏常熟Ms5.1级地震前连云港与常熟及连云港与溧阳的地磁幅相法瞬时差幅度,成功地提取了震前异常。 相似文献
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地磁Z分量日变"低点位移"异常成因分析 总被引:2,自引:0,他引:2
本文基于对地磁Z分量日变"低点位移"异常和太阳静日变化内外源场等效涡旋电流体系时空演化特征的分析,提出了"电磁炉效应"假说,以解释地磁Z分量日变"低点位移"异常的成因.本文认为,起源于地球内部和外部涡旋电流体系所产生的太阳静日变化Sq,作为一个持续的交变磁场,切割地壳深部的高导低速层,形成涡旋电流并产生热能,致使高导低... 相似文献
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The diurnal-variation anomalies of the vertical-component in geomagnetic field are mainly the changes of phase and amplitude
before strong earthquakes. On the basis of data recorded by the network of geomagnetic observatories in China for many years,
the anomalous features of appearance time of the minima of diurnal variations (i.e, low-point time) of the geomagnetic vertical components and the variation of their spatial distribution (i.e, phenomena of low-point displacement) have been studied before over 30 strong earthquakes with M
S≥6.6 such as Kunlunshan M
S=8.1 earthquake on November 14, 2001; Bachu-Jashi M
S=6.8 earthquake on February 24, 2003; Xiaojin M
S=6.6 earthquake on September 22, 1989, etc. There are good relations between such rare phenomena of geomagnetic anomalies and the occurrence of earthquakes. It has
been found that most earthquakes occur in the vicinity of the boundary line of sudden change of the low-point displacement
and generally within four days before and after the 27th or 41st day counting from the day of appearance of the anomaly. In
addition, the anomalies of diurnal-variation amplitude near the epicentral area have been also studied before Kunlunshan M
S=8.1 earthquake and Bachu-Jiashi M
S=6.8 earthquake.
Foundation item: National Science Technology Tackle Key Project during the Tenth Five-year Plan (2001BA601B01-05-04) 相似文献
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Introduction The occurrence of earthquake has relations not only with seismogenic process of source area,but also with the environment of inner (earth space) and outer (earth-sun space). The varyinggeomagnetic field is natural medium that connects with both factors (DING, 1988). There are two kinds of basic ideas using the diurnal-variation anomalies of the verti-cal-component (Z) in geomagnetic field to predict earthquake. The first kind is local geomagneticanomalies that are obta… 相似文献
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地磁低点时间在空间分布上的主要特征是随着经度变化而变化。为了求出这种变化关系的解析式,首先使用国家地磁台网的数据计算甘肃省近三年13个地磁台站的低点时间序列和低点时间的期望,并绘制了低点时间序列的频次分布图和概率密度曲线;然后对低点时间与台站经度的关系做线性回归,并指出这个线性回归方程应无限趋近于“格林尼治时间-经度”关系式。文章第一次提出台站经度与地磁Z分量低点时间的关系式,并提出它的趋近方程。各台站低点时间的期望就是地磁低点时间的正常背景值,它是判定地磁低点时间异常与否的参考标准。本文的工作完善和发展了丁鉴海先生的地磁低点位移法。 相似文献
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This paper analyzes the distribution characteristics of geomagnetic low-value displacement in Gansu and its adjacent areas from 1995 to 2003 on the basis of the data of the daily amplitude minimum value time of the geomagnetic vertical component. It is shown that in addition to the changing rules of geomagnetic low-value displacement itself, there is a better correlation between geomagnetic low-value displacement and the occurrence of moderately strong earthquakes. There appeared to be geomagnetic low-value displacement before the moderately strong earthquakes in Gansu in the 9 years from 1995 to 2003. This result indicates that geomagnetic low-value displacement is of instructive significance for earthquake prediction to some extents. 相似文献
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2010年1月11-24日,华北地区出现7次地磁低点位移异常。异常结束1天后研究区内发生2010年1月24日山西河津4.8级地震。采用实测低点时间减去理论低点时间的方法剔除低点时间经度效应,并以剔除经度效应后低点时间为0 h的等值线作为低点位移分界线,山西河津4.8级地震震中处于1月16日、17日、19日、22日地磁低点位移分界线上。低点位移异常日期间,华北地区存在显著的高梯度带,该文采用梯度值定量描述低点时间空间变化程度。在正常日期间,华北地区未出现梯度值大于1 h/(°)的区域,在异常日期间,出现梯度值大于1 h/(°)的区域,河津4.8级地震多位于高梯度区边缘。 相似文献