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Episodic Tremor and Slip in Northern Sumatra Subduction Zone

机译:苏门答腊北部郊区震动和滑动

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The first reported observation of non-volcanic tremor in Sunda Arc in Sumbawa, Indonesia open a possibility of discovery of episodic tremor and slip (ETS) from out of Pacific Rim. Non-volcanic tremor gives some important information about dynamic of plate boundaries. The characteristics of these tremors are visually as non-impulsive, high frequency, long-duration and low-amplitude signals. Tectonic tremor occurred in a transition part of brittle-ductile of a fault and frequently associated with the shearing mechanism of slow slip. Tectonic tremor is a seismic case that also very interested, because it shows strong sensitivity to stress changes. Deep non-volcanic tremor is usually associated with episodic slow-slip events. Tectonic tremor is found in close association with geodetically observed slow-slip events (SSE) in subduction zones. One research found that there is possibility of SSE occurrence on Banyak Islands, North Sumatra revealed from coral observation. The SSE occurred on the Banyak Islands portion of the megathrust at 30-55 km depth, within the downdip transition zone. We do a systematic search of episodic tremor and its possible relationship with slow-slip phenomena in Northern Sumatra subduction zone. The spectrogram analysis is done to analyze the potential tremor signals. We use three component broadband seismic stations with 20, 25, and 50 sampling per second (BH* and SH* channels). We apply a butterworth 5 Hz highpass filter to separate the signal as local tremor and teleseismic/regional earthquakes. Before computing spectrogram to avoid high-frequency artifacts to remote triggering, we apply a 0.5 Hz filter. We also convert the binary seismic data into sound waves to make sure that these events meet the tectonic tremor criterion. We successfully examine 3 seismic stations with good recording i.e. GSI, SNSI and KCSI. We find there are many evidences of high frequency episodic tremor like signals. This include an analysis of potential triggered trem
机译:首次报道了在Sunda弧中的非火山震颤在Sunda弧中的观察,印度尼西亚在太平洋边缘开辟了发现的情节震颤和滑动(ETS)的可能性。非火山岩震颤给出了有关板界动态的重要信息。这些震颤的特征在视觉上作为非冲动,高频,长持续时间和低幅度信号。构造震颤发生在故障的脆性韧性的过渡部分,并且经常与慢速滑动的剪切机构相关联。构造震颤是一种非常感兴趣的地震案例,因为它表现出对压力变化的强烈敏感性。深度非火山岩震颤通常与情节速滑事件相关联。在俯视区域中与地理上观察到的慢速速度事件(SSE)密切相关的构造震颤。一项研究发现,北苏门答腊从珊瑚观测揭示了丹尼亚克群岛的SSE发生。 SSE在梅吉坦邦岛的部分在30-55公里深度,在下楼的过渡区内。我们对北部苏门答腊郊区的速度震颤和缓冲现象进行了系统搜索。进行频谱图分析以分析潜在的震颤信号。我们使用具有20,25和50个采样的三个组件宽带地震站(每秒50个采样(BH *和SH *通道)。我们应用Butterworth 5 Hz高通滤波器,将信号分离为当地震颤和Teleismic /地区地震。在计算频谱图之前,以避免高频伪像远程触发,我们应用0.5 Hz过滤器。我们还将二进制地震数据转换为声波,以确保这些事件符合构造震颤标准。我们成功地检查了3个地震站,良好的录音即,GSI,SNSI和KCSI。我们发现有很多关于信号的高频焦震颤的证据。这包括对潜在触发的触发的分析

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