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分布式光纤高密度地震观测揭示门源M_(S)6.9地震余震活动与隐伏断层 被引量:2
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作者 包丰 曾祥方 +3 位作者 林融冰 迟本鑫 吕昊 沙成宁 《科学通报》 EI CAS CSCD 北大核心 2022年第27期3340-3347,共8页
高密度的地震观测台阵对地震监测和结构成像都具有重要意义,利用分布式光纤地震传感技术结合现有通讯光缆可以快速构建高密度地震监测网.2022年门源M_(S)6.9地震发生后,利用震中区20.8 km通讯光缆构建了间距10 m的高密度地震台阵,记录... 高密度的地震观测台阵对地震监测和结构成像都具有重要意义,利用分布式光纤地震传感技术结合现有通讯光缆可以快速构建高密度地震监测网.2022年门源M_(S)6.9地震发生后,利用震中区20.8 km通讯光缆构建了间距10 m的高密度地震台阵,记录到了丰富的余震信号.发展了地震自动检测算法,并在3天观测中检测到了166个余震,与固定台网目录形成互补.在高密度地震波场记录中识别出多个断层相关信号,推测其为断层散射波,由此发现了门源盆地内部的多个断层.研究表明,分布式光纤地震传感技术结合地震自动检测算法和波场分析技术可以为发震趋势判断及隐伏断层探测提供可靠参考的数据,在高原重要基础设施沿线的地震灾害研究中具有良好的应用前景. 展开更多
关键词 门源地震 分布式光纤地震传感 高密度地震台阵 余震监测 断层探测
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Source-Independent Amplitude-Semblance Full-Waveform Inversion using a Hybrid Time-and Frequency-Domain Approach
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作者 benxin chi Lianjie Huang 《Communications in Computational Physics》 SCIE 2020年第6期328-341,共14页
Full-waveform inversion is a promising tool to produce accurate and high-resolution subsurface models.Conventional full-waveform inversion requires an accu-rate estimation of the source wavelet,and its computational c... Full-waveform inversion is a promising tool to produce accurate and high-resolution subsurface models.Conventional full-waveform inversion requires an accu-rate estimation of the source wavelet,and its computational cost is high.We develop a novel source-independent full-waveform inversion method using a hybrid time-and frequency-domain scheme to avoid the requirement of source wavelet estimation and to reduce the computational cost.We employ an amplitude-semblance objective function to not only effectively remove the source wavelet effect on full-waveform inver-sion,but also to eliminate the impact of the inconsistency of source wavelets among different shot gathers on full-waveform inversion.To reduce the high computational cost of full-waveform inversion in the time domain,we implement our new algorithm using a hybrid time-and frequency-domain approach.The forward and backward wave propagation operations are conducted in the time domain,while the frequency-domain wavefields are obtained during modeling using the discrete-time Fourier trans-form.The inversion process is conducted in the frequency domain for selected frequen-cies.We verify our method using synthetic seismic data for the Marmousi model.The results demonstrate that our novel source-independent full-waveform inversion pro-duces accurate velocity models even if the source signature is incorrect.In addition,our method can significantly reduce the computational time using the hybrid time-and frequency-domain approach compared to the conventional full-waveform inversion in the time domain. 展开更多
关键词 Amplitude semblance full-waveform inversion hybrid time and frequency domain source independent source wavelet
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