Research on the Seismic Wave Characteristics of Low Frequency Signals before the Alxa Left Banner MS5.8 Earthquake in Inner Mongolia, China     

Liang Shash  Gao Lixin  Dai Yong  Ge Gen  Wang Lei 《中国地震研究》2018,32(3):367-376

In order to search for the seismic wave characteristics of low frequency signals in the Alxa Left Banner region,Inner Mongolia,the low frequency signals of seismic wave data are extracted from the earthquakes of MS5. 8 in 2015 and MS5. 0 in 2016 in this area. The results show that:① Before the MS5. 8 earthquake,the seismic stations located near the epicenter in Wuhai,Dongshengmiao,and Shizuishan recorded seismic waves that showed the phenomenon of spectrum shift from high to low frequency.② The low frequency signals recorded by different stations have obvious difference.③ According to the data recorded by the station closest to the epicenter,low-frequency signals were recorded about120 hours before the earthquake and had obvious anomalies. This may reflect slow slip before the earthquake.  相似文献   

Mallat算法在数字地震信号压缩中的应用   总被引：1，自引：1，他引：0  

王军 《地震地磁观测与研究》2017,38(5):133-138

地震台站多、数据采集量大,日产出数据量庞大,研究数字地震信号的压缩方法成为行业热门课题。尝试将Mallat算法应用于数字地震波形数据压缩。选取不同的小波分解函数,对不同类型的数字地震信号进行3—5层的小波分解,将得到的小波系数进行分层硬阈值重构运算,对原始信号和处理信号进行压缩。分析可知,Mallat算法压缩比更高,与原始信号相比,重构信号不失真、能量保留系数高。  相似文献   

全张量磁梯度数据解释的均衡边界识别及深度成像技术   总被引：2，自引：0，他引：2       下载免费PDF全文

舒晴  马国庆  刘财  李丽丽 《地球物理学报》2018,61(4):1539-1548

全张量磁梯度数据具有高精度、高分辨率、多参量的优点,能更加清晰地刻画地质体的分布特征,综合利用磁张量梯度数据准确地获得地质体水平位置和深度信息是解释的主要目的.磁张量数据的方向解析信号具有减小倾斜磁化干扰的优点,常被用来圈定磁源体的水平位置,但解析信号强度随着地质体埋深的增加急剧衰减,难以有效识别较深的地质体.张量数据均衡边界识别技术,利用不同方向解析信号的比值函数,能有效地均衡不同深度地质体的响应,同时显示不同深度地质体的边界,提高了对较深地质体的分辨率.磁张量数据深度成像技术根据实测张量数据与假定模型张量数据的相关系数来给定地质体的深度,综合利用多参量数据联合反演提高了反演结果的准确性,且无需进行复杂的反演运算,是大数据量张量数据解释的有效方法.理论模型试验证明：磁张量数据均衡边界识别技术可清晰和准确地识别地质体的水平范围,受倾斜磁化干扰小;磁张量数据深度成像技术可准确地获得地质体的深度信息,具有较强的抗噪性.将上述方法应用于铁矿区实测航磁张量梯度数据解释,获得了铁矿体水平分布与埋深,深度结果与张量欧拉反褶积法计算结果一致.  相似文献   

基于分数阶小波域GSM模型的地震信号随机噪声压制方法          下载免费PDF全文

汪金菊  李青  徐小红  曹丽 《地球物理学报》2018,61(7):2989-2997

地震信号中的随机噪声是一种干扰波,严重降低了地震信号的信噪比,并影响着资料的后续处理和分析.本文根据地震信号中有效信号和随机噪声的差异,结合分数阶B样条小波变换与高斯尺度混合模型提出了一种地震信号随机噪声压制方法.首先利用分数阶B样条小波变换将含噪地震信号映射到最优分数阶小波时频域内,然后对各小波子带系数分别建立高斯尺度混合模型,由贝叶斯方法估计出源地震信号小波系数,最后使用分数阶B样条小波逆变换重构得到降噪后的地震信号.利用本文方法对合成地震记录和实际地震信号进行降噪处理,实验结果表明本文方法能够有效地压制地震信号中的随机噪声,并且较好地保留了有效信号.  相似文献   

利用分段时频峰值滤波法抑制磁共振全波信号随机噪声          下载免费PDF全文

林婷婷  张扬  杨莹  杨玉晶  滕飞  万玲 《地球物理学报》2018,61(9):3812-3824

磁共振信号极其微弱,容易受到周围环境中各种电磁噪声干扰.其中随机噪声,由于频带宽、不规则、无规律、与有效信号混叠,难以抑制.近年来,采用数量级为10⁴~10⁵ Hz采样频率收录的全波磁共振信号,以其携带丰富全面的信息量,为数据处理及解释提供了更多的潜能.然而,只要随机噪声的幅度大于信号幅度,拟合得到的信号特征参数准确度就会降低.目前普遍采用的数据叠加方法仅能抑制部分随机噪声,且需要多次采集信号,探测效率低.本文针对全波磁共振信号采样点数多和信号非线性强的特点,提出采用分段时频峰值滤波（STFPF）法消噪,将全波磁共振信号分成若干段,编码为解析信号的瞬时频率,采用短窗长PWVD计算解析信号的时频分布,利用时频分布沿瞬时频率集中的特性,通过提取时频分布的峰值获得信号的无偏估计,达到抑制全波磁共振信号随机噪声的目的.为了验证消噪效果,与传统叠加法进行对比分析,仿真结果表明,对于单次采集信号,信噪比低至-5 dB时,STFPF方法依然能有效抑制信号中的随机噪声,消除随机噪声后信噪比提高23.19 dB,信号的初始振幅拟合误差为3.03%,平均横向弛豫时间拟合误差为2.7%,消噪效果优于传统叠加法,且由于无需多次采集磁共振信号,可有效提高探测效率.模型数据的反演解释进一步验证了STFPF方法的有效性,本文研究结果为实际数据处理奠定了良好的基础.  相似文献   

Time‐phase amplitude spectra based on a modified short‐time Fourier transform          下载免费PDF全文

Gulan Zhang 《Geophysical Prospecting》2018,66(1):34-46

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Ocean surface current retrieval and imaging with a new shore-based X-band radar based on time-shifted up-and-down linear frequency modulated signal     

Yijun He  Xin Song  Baochang Liu  Na Yi  Xiuzhong Li 《海洋学报(英文版)》2021,40(3):112-121

This paper proposes a multifunction radar that can not only measure sea currents but also perform sea-surface imaging. The fundamental aspect of the proposed radar comprises transmitting time-shifted up-and-down continuous wave linear frequency modulated signals that allow for the offset of two one-dimensional range images of the sea surface that respectively correspond to the upward linear frequency modulated(LFM) signal and the downward LFM signal. Owing to the Doppler frequency shift from the sea surface, a range offset, which is proportional to the radial velocity of the sea surface, occurs between the upward and downward LFM signals. By using the least-squares linear fitting method in the transformed domain, the range offset can be measured and the current velocity can be retrieved. Finally, we verify the accuracy of current measurement with simulation results.  相似文献   

新源、和静交界M_L6.8级地震序列应力降和震源机制研究     

刘建明  王琼  刘杰  邓菲  向元  杨文  李金 《中国地震研究》2017,31(1):25-38

Based on the digital waveform data recorded by Xinjiang Digital Seismic Network for the Xinyuan-Hejing M_L6.8 earthquake sequences of June 30,2012,this paper analyzes the stress drops of earthquake sequences and the correlation coefficients of focal mechanisms significant for strong aftershocks.Firstly,the source parameters of the Xinyuan-Hejing M_L6.8 earthquake sequences are obtained by applying the spectrum analysis and the Brunes source model.Then,the correlation coefficients of spectral amplitudes are calculated using the low-frequency spectral amplitude recorded by the same station for the different events.Finally,based on the results of the correlation coefficients of spectral amplitudes,the events with similar focal mechanisms are grouped using the clustering method.The results show that:(1)The stress drop values show a steady trend in the aftershock sequence calm period and the stress drop values show a rise-fall in strong aftershocks.(2)The moving average correlation coefficient of amplitude spectrum begins to spread after the main shock.It shows that the correlation decreases between the main shock and the aftershocks in mechanisms.(3)The results of focal mechanism groups show that the earthquake sequences are mainly strike slips.The stress distribution of the main pressure axis is nearly NS,which is the same as the structural stress field.(4)The magnitude and mechanism show that there is an agreement before the strong aftershock,which shows that the regional stress field is enhanced.  相似文献   

Seismic energy dissipation under variable amplitude loading for rectangular RC members in flexure          下载免费PDF全文

《地震工程与结构动力学》2018,47(4):831-853

The energy dissipation characteristics of reinforced concrete members that exhibit both strength and stiffness deterioration under imposed displacement reversals were investigated. To do this, 24 symmetrically reinforced concrete rectangular specimens were tested under stable variable and random variable amplitude inelastic displacement cycles. Stable variable amplitude tests were employed to determine the low‐cycle fatigue behavior of specimens where the loading sequence was the major variable. A 2‐parameter fatigue model was developed in order to express the variation of the dissipated energy in displacement cycles with the cumulative hysteretic energy. This model was then used to predict the energy dissipation of test specimens subjected to random variable amplitude displacement cycles simulating severe seismic excitations. It has been demonstrated that the remaining energy dissipation capacity for the next displacement cycle was dependent on the relative relationship between the maximal displacement cycle and the energy dissipated along the completed displacement path. The plastic energy dissipation capacity of reinforced concrete members is both displacement path dependent and cumulative hysteretic energy dependent.  相似文献   

Loran-C信号中直达波与反射波的提取方法研究          下载免费PDF全文

黄显良  戚浩  郁建芳  谢石文  王琐琛  杨波  夏仕安 《地震工程学报》2017,39(4):662-666

Loran-C信号中直达波和反射波到时差的提取是利用其进行测距的关键所在。通过分析Loran-C信号实测波形与理论波形的特征,认为两者所包含的直达波信号一致。基于此特征,通过波形相减的方法从实测Loran-C信号中剔除理论直达波信号,并结合互相关方法求解出直达波和反射波的到时差。  相似文献