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| 喀什基准台宽频带井下和地表地震计记录数据对比研究 |
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赵瑞胜1, 危自根2,3, 闫新义4, 黄瑜1
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1.新疆维吾尔自治区地震局喀什地震监测中心站, 新疆喀什 844000;2.中国科学院精密测量科学与技术创新研究院, 大地测量与地球动力学国家重点实验室, 武汉 430077;3.中国地质科学院地质研究所, 自然资源部深地动力学重点实验室, 北京 100037;4.新疆维吾尔自治区地震局, 乌鲁木齐 830011
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| 摘要: |
| 对比分析喀什基准台麦盖提井下和相邻地表宽频带地震计记录的背景噪声、麦盖提ML3.1近震和棉兰老岛ML6.6远震波形记录以及功率谱，并进一步研究了相关的震级差和台站下方结构。研究结果表明，井下和地表地震计记录到的波形特征和功率谱既存在相似性，又具有差异性；井下地震计记录的近、远震波形更清晰、简洁，且功率谱也相对较低。麦盖提台站下方地壳厚度约50km，井下地震计下方59m和地表地震计下方47m深度范围内的平均S波速度分别为0.59km/s和0.47km/s。井下地震计得到的近震和远震震级分别比地表地震计得到的震级小0.518和0.025。本文研究结果对合理布设地表和井下地震计，以及利用其观测数据进行地震学研究具有一定的指示意义。 |
| 关键词: 井下和地表地震计 功率谱 近震和远震 RZ比 震级差 接收函数H-κ叠加 |
| DOI： |
| 分类号:P315 |
| 基金项目:新疆地震科学基金(202123)、自然资源部深地动力学重点实验室开放研究课题(J1901-16)共同资助 |
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| Earthquake Waveform Comparison of Broadband Records between Borehole and Ground Seismometers in Kashi Seismic Station |
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Zhao Ruisheng1, Wei Zigen2,3, Yan Xinyi4, Huang Yu1
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1.Kashi Earthquake Monitoring Center of Earthquake Agency of Xinjiang Uygur Autonomous Region, Kashi 844000, Xinjiang, China;2.State Key Laboratory of Geodesy and Earth's Dynamics, Innovation Academy for Precision Measurement Science and Technology, Chinese Academy of Sciences, Wuhan 430077, China;3.Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China;4.Earthquake Agency of Xinjiang Uygur Autonomous Region, Urumqi 830011, China
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| Abstract: |
| We analyzed and compared the waveforms and power spectrums of background noise of Maigaiti ML3.1 and Mindanao ML6.6 earthquakes recorded by broadband seismometers in borehole and at ground in Maigaiti seismic station in Kashi. We further studied the amplitude differences and structure beneath the Maigaiti station based on the records from borehole and ground seismometers. The results show a more clear and concise waveforms of earthquakes and lower power spectrum recorded by the borehole seismometer and coexistence of both similarity and difference between the waveforms and power spectrums. The crustal thickness is 50km beneath the Maigaiti station. The average S-wave velocities at a range of 0~59m deep beneath the borehole seismometer and 0~47m deep beneath the ground seismometer are 0.59km/s and 0.47km/s, respectively. The magnitudes of local earthquake and teleseism obtained by borehole seismometer are 0.518 and 0.025 smaller than those obtained by ground seismometer, respectively. The results obtained in our studies are useful to the deployment of ground and borehole seismometers as well as seismic study by using their observational data. |
| Key words: Borehole and ground seismometers Power spectrum Local earthquake and teleseism RZ ratio Magnitude difference H-κ stacking of receiver function |
