论文标题
2013年深奥霍茨克地震的余震
Aftershocks of the 2013 deep Okhotsk earthquake
论文作者
论文摘要
强烈的深层地震发生在2013年5月24日在Okhotsk海上，UTC 05:44。地震的大小为M = 8.3，低中心的深度为629 km。地震伴随着深焦点的余震。该论文致力于研究余震的时空特性。估算了地震源的停用系数，该系数在主要冲击后“冷却”。发现了地球的环形振荡对余震的调节。考虑了有关圆世界地震回声的问题和上级时空分布的肋骨结构。关键字：Omori法律，停用系数，反问题，调制，自由振荡，圆世界回声，时空分布
Strong deep earthquakes occurred in the Sea of Okhotsk, May 24, 2013 at 05:44 UTC. The magnitude of the earthquake is M = 8.3, the depth of the hypocenter is 629 km. The earthquake was accompanied by the deep-focus aftershocks. The paper is devoted to the study of the space-time properties of aftershocks. An estimate is made of the deactivation coefficient of the earthquake source, which "cools down" after the main shock. The modulation of aftershocks by toroidal oscillations of the Earth was discovered. The questions about the round-the-world seismic echo and the ribbed structure of the spatio-temporal distribution of epicenters are considered. Keywords: Omori law, deactivation coefficient, inverse problem, modulation, free oscillations, round-the-world echo, space-time distribution
