共查询到19条相似文献，搜索用时 166 毫秒
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《地球物理学进展》2020,(2)
本文利用极化方法,提取和分析新疆区域2008—2017年拥有秒采样数据的乌鲁木齐、喀什、且末、温泉4个台站的垂直幅度极化值,分析极化值异常与新疆及其邻区2008年以来6级以上地震的关系.地磁场观测较容易受到高空电流体系等外源场的影响,为了分析外源场对极化值的影响,统计了2008—2017年共计64次磁暴期间的极化值,4个台站磁暴期间极化值都非常小,除了温泉台有1次大于2倍均方差之外,其余全部都小于各个台站的2倍均方差(极化值异常初始阈值为3倍均方差),同时通过计算出的极化值与K_p指数的相关系数可以看出,4个台站的相关系数都非常小(小于0.2),基本可以判断极化值在磁场扰动时应该表现为低值,而大量研究表明地震之前极化值会出现高值异常,因此基本排除了外源场对极化值的影响.2008—2017年共计93次5级以上地震,因各个台站背景噪声和仪器噪声以及构造背景差别较大,计算出的极化值幅度差别较大,各个台站极化值之间不具有可比性.结果表明:当各个台站的震中距相当时,震级越大,异常幅度越大.喀什台由于与多国交界,地质构造环境更为复杂,异常幅度等显示出更为复杂的特性,因此漏报等情况也较多. 相似文献
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基于甘青川地区的14个地磁台站秒采样资料,对2022年1月8日青海门源MS6.9地震前地磁垂直强度极化异常的时空变化特征进行分析研究。计算结果显示,在2021年10月底出现了地磁极化超阈值高值异常变化,异常台站主要分布在青海、甘肃和四川地区,异常出现后73天发生了门源地震,震中位于极化高值异常阈值线附近。研究还发现,此次地磁极化异常具有一定的时空变化特征,时间上,不同台站极化异常具有较好的时间同步性;空间上,极化异常高值区呈现出沿震中附近出现后不断扩展最终再向震中收缩的特点。此外,各地磁极化异常台站的归一置零极化值、异常持续时间与震中距存在较好的负相关性,异常台站距离地震震中越近,其归一置零极化值越高,异常持续时间也越长,这一特征符合地震电磁扰动信号的衰减特征。根据极化异常和地震的时空关系分析认为,此次地磁极化高值异常对应了之后在异常高值区边缘发生的门源MS6.9地震。 相似文献
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2022年1月8日青海门源县发生6.9级地震,此次地震前青海地区出现了大量地球物理观测异常。2021年10月下旬青海地区出现地磁垂直强度极化高值异常,10月27日异常台站最多,并在门源-祁连至兴海地区形成一个面积约为6.6×104km2的高值异常区;此外,2021年7—11月青海地区8项地下流体观测数据出现准同步异常变化。结合青海及周边地区历史震例的分析结果,认为2021年11月23日至2022年1月23日,青海西北部地磁垂直强度极化高值区内可能发生5.6～6.4级地震。门源6.9级地震发生在地磁垂直强度极化异常出现后的73天,震中位于预测区的边缘,地震的发生时间和地点与预测意见一致,但震级超出预测意见上限值0.5级。此次地震前基于地球物理观测地震预测指标体系开展的短临异常跟踪分析过程,对中国大陆西部地震预报工作具有一定的参考意义。 相似文献
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对2017年8月8日九寨沟7.0级地震前后四川及其邻区地磁台站数据进行垂直强度极化方法计算, 使用5~100 s周期发现震前地磁极化计算结果存在如下的显著异常特征: ① 2017年3月震中附近地磁台站同步存在极化超阈值异常, 时间上显示为短期异常; ② 同步异常台站出现最大幅度的时间较一致; ③ 九寨沟地震发生在异常阈值线附近, 对该方法预测地点有一定指示意义; ④ 对比异常时段内的Dst指数, 认为此次同步超阈值异常不是空间电流体系所造成的; ⑤ 3月18日地磁台站出现极化异常的台站数量较多, 异常分布区域面积较大, 异常主要集中在西北地区可能反映了该区域的应力作用。 相似文献
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采用极化分析方法处理地磁秒数据.对不同台站地磁秒数据进行分析发现,极化值在地震发生前约2个月内有明显异常,且在傅里叶频谱上表现不太明显.另外,不同地磁分量的极化值映震效果不同,大部分震例极化值升高、振幅增大,小部分震例极化值低值、平稳.研究认为,该方法可以用于地磁秒数据震磁异常信息提取. 相似文献
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甘-青地区地磁垂直分量加卸载响应比、逐日比分析 总被引：3，自引：0，他引：3
《华南地震》2015,(3)
以甘肃、青海及周边地区(30.5°~41.0°N,94.0°~108.0°E)作为研究区域,采用地磁垂直分量加卸载响应比方法,以及由此演化出的地磁垂直分量逐日比方法,对位于甘-青地区的都兰、山丹、古丰、固原和中卫五个台站地磁数据进行处理。结果显示:1自2008年以来,甘-青地区累计发生5次显著地震,其中4次地震前10个月内,出现过加卸载比成组高值异常,3次地震之前10个月内出现过逐日比成组高值异常;2甘-青地区地磁垂直分量加卸载响应比、逐日比异常判据阈值分别为3.0、2.8。 相似文献
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利用2016—2018年3期华北地区流动地磁矢量原始测量资料, 经数据计算获得2期华北地区和张家口—渤海地震活动带及邻区岩石圈磁场时空变化模型。 研究结果显示: 张家口—渤海地震带岩石圈磁场变化空间分布不均匀, 具有明显的分区特征, 在张家口段(西段)与北京段(中西段)分界处和北京段(中西段)与唐山段(中东段)分界处岩石圈磁场各要素具有明显的异常变化, 如水平矢量存在转向和幅值变化, 磁偏角与磁倾角具有正负异常高梯度带的特征, 这与张家口—渤海地震带构造分段性特征密切相关。 张家口—渤海地震带位于燕山块体与华北平原块体之间, 两者运动的平动速率之差是张家口—渤海地震带左旋走滑的直接动力来源, 而各断裂带左旋走滑速率之差很可能是岩石圈磁场空间变化分段性分布的主要原因。 相似文献
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Diurnal characteristics of geoelectric fields and their changes associated with the Alxa Zuoqi M_S5.8 earthquake on 15 April 2015(Inner Mongolia) 
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下载免费PDF全文 In China, efforts are being made to monitor geoelectric fields through a large network of stations deployed and managed by the China Earthquake Administration. The diurnal variations in the geoelectric field waveforms were similar in the quiet magnetic periods when K5(generally, K3 indicates a quiet time). The arrival time points of the maxima in the geoelectric field waveforms exhibited differences in local time related to geographic longitude. The amplitude of diurnal variation was several to 16.6 mV/km and decreased with increasing latitude. Further,the amplitude of diurnal variation, which was related to seasonal changes, was larger in summer and autumn than in spring and winter. The periods of diurnal changes during quiet days were 24, 12, 8, 6, 4 hours and several minutes over large areas. Finally, the observed diurnal variations in geoelectric field prior to the Alxa Zuoqi M_S5.8 earthquake on 15 April 2015 were studied, and pronounced changes in the spectral values of the geoelectric fields were found to be associated with the Alxa Zuoqi earthquake in Inner Mongolia. 相似文献
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N. A. Zolotukhina 《Geomagnetism and Aeronomy》2010,50(8):963-969
A comparative analysis of extremely low frequency waves registered by Cluster satellites after a sudden impulse (SI) and the
following substorm onset (SO) at distances L ∼ 4 from the Earth’s center was performed. It was shown that both phenomena in the equatorial morning magnetosphere activated
magnetic field oscillations of periods from 40 to 200 s. Oscillations accompanying SI and SO were found to be of similar spectral
composition but different polarizations. The differences in polarization became well-pronounced near the main spectral maximum
(100–130 s), where the transition from SI to SO was accompanied by reverse of rotation of the magnetic field disturbance vector
and by reorientation of the oscillation polarization ellipse. 相似文献
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本文根据自由核章动在章动观测和时变重力观测中引起的与其频率相近的受迫章动项或固体潮潮波的共振特性,选取6个不同机构解算的VLBI天极偏差序列和全球超导重力仪网络提供的7个台站高精度时变重力观测资料,根据加权最小二乘方法拟合地球自由核章动参数,研究其本征周期的时间变化特征.VLBI资料获得的本征周期变化幅度在1天之内,存在十年尺度的时间变化特征,迭积多台站同时段重力资料获得的自由核章动本征周期时变特征与VLBI获得的结果相比变化幅度较大,但趋势大致符合.在此基础上,通过自由核章动的理论模型探讨了影响其本征周期的几个主要因素,结果表明FCN周期变化与电磁耦合存在相关性,核幔边界磁感应强度径向分量变化导致的电磁耦合的变化可能是造成FCN周期时变性的原因. 相似文献
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河北省数字地电场数据分析 总被引：13，自引：0，他引：13
通过分析总结河北省数字地电场的正常场和异常信息，发现正常记录除了显示日变周期外，还记录到了半日和三分之一日周期，比较长的周期还有半月周期等；干扰信息主要与电极极化及磁暴等有关，大磁暴干扰一般会出现高频信号，破坏正常日变形态，其主要表现为多台同步等幅信号；对台站的电场方向性研究发现，在正常时段电场记录方向性显著，而磁暴记录期内方向性较差，显示外空异常源方向比较复杂。最后对一些可能与地震有关的异常现象进行了分析探讨。我们认为，目前的多极距地电场观测对排除干扰及异常识别带来很大方便，但共用电极的观测方式为异常识别增加了障碍。 相似文献
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During the seismovolcanic crisis of 1976–1977 at La Soufrière on Guadeloupe, a magnetic network of 12 reference markers was set up. Measurements of the intensity of the earth's magnetic field, carried out up to once a day at each marker, showed volcano-magnetic variations of several nanoteslas (nT). The variations, at certain markers, were more or less concealed by transient magnetic variations due to anomalies in conductivity. As early as 1978, measurements were resumed and a telemetering network was coupled with the network of reference markers, to which 4 new markers were added. A detailed study of conductivity anomalies was carried out on the entire volcano. Contrasts in conductivity linked to the existence of a superficial conducting surface, on a SSW/NNE axis, located south of the volcano, caused a great lack of homogeneity in the field variations measured at the surface. Variations greater than about 10 nT appeared in the difference in intensity of the earth's magnetic field between two stations.No long-term magnetic variation was observed between 1978 and 1984. On the network of markers, the accuracy of measurements of volcanic effects was at best 2 nT. Measurements carried out on the telemetering network during the night refined these results, since their accuracy was 1 nT. The only significant volcanic crisis between 1978 and 1984 (5–7 January 1981) seems to be observed by telemetering stations. All the measurements carried out in periods of volcanic inactivity make it possible to re-examine the crisis of 1976–1977. Though volcanomagnetic effects over short periods cannot be accurately determined, variations with a time constant of several weeks were present over the entire volcano. These variations were as high as 7–8 nT in remote stations and they can be linked to the three major phases of eruptive activity at La Soufrière during the crisis of 1976–1977. 相似文献
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利用延庆地震台2004年地电场的观测资料,研究其变化情况,分析引起其变化的具体原因,结果表明:延庆地震台地电场的观测容易受到磁暴、雷雨等干扰,电极的极化影响最为严重,这些因素给地电场震前中短期异常的识别带来了困难,但是从短期来看,地电场观测精度较高,对场地的电磁变化反映比较灵敏。 相似文献
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Summary The harmonically variable magnetic field, generated by a tangential magnetic dipole (TMD), located eccentrically at the surface of the Earth's core, is investigated for various periods of time variations and for a three-layer conductivity model of the Earth. Numerical computations have shown that the field is inductively damped for variation periods of less than 500 years as compared to the field of a static TMD. It is proved that the field appropriate to the TMD, has a more complicated distribution of the Earth's surface than the field of a radial magnetic dipole. Comparison with maps of the non-dipole part of the geomagnetic field shows that the TMD is not as suitable for interpreting the observed non-dipole field and its variations as the eccentric radial magnetic dipole. 相似文献