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Spheroidal oscillations of the Earth stimulated by the Sumatra-Andaman earthquake with CDSN data

机译:苏门答腊-安达曼地震刺激的地球球状振荡与CDSN数据

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The 0S2~0S54 spheroidal modes of Earth's free oscillations, triggered by the great Sumatra-Andaman earthquake of 26 December 2004 are retrieved from VHZ data recorded by seven upgraded stations of China Digital Seismograph Network (CDSN). We compare these spheroidal modes with theoretical free oscillation spectra calculated from the Preliminary Reference Earth Model (PREM) and find a coincidence between their periods. Spectral splitting phenomenon is observed obviously in 0S2, 0S3, 0S4, 2S1 and 1S2 free oscillation modes. What is most noticeable is that the oscillation mode 2S1 is reported for the second time (the first time by Rosat et al) without any data stacking. We simulated the split singlet of 0S2 mode on seven CDSN stations based on general focal mechanism and seismic moment of the earthquake. The result shows that seismic moment of the earthquake can reach 1023 N·m. We also find that the recording of Earth's free oscillations carries abundant information of source mechanism and earthquake location, which is applicable to the detailed study of source rupture parameters.
机译:2004年12月26日苏门答腊-安达曼大地震引发的地球自由振荡的0S2〜0S54球形模式,是从中国数字地震台网(CDSN)的七个升级台站记录的VHZ数据中检索得到的。我们将这些球面模式与根据初步参考地球模型(PREM)计算出的理论自由振动谱进行比较,并发现它们的周期之间存在重合。在0S2、0S3、0S4、2S1和1S2自由振荡模式中明显观察到光谱分裂现象。最值得注意的是第二次报告振荡模式2S1(Rosat等人第一次报告),没有任何数据堆叠。基于地震的一般震源机制和地震矩,我们在七个CDSN站上模拟了0S2模式的分裂单峰。结果表明,该地震的地震矩可以达到1023 N·m。我们还发现,记录地球的自由振荡携带了丰富的震源机制和地震位置信息,适用于震源破裂参数的详细研究。

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